T W Reader geological photographs, long excursions 1914. Part 2 - index, GA 'Carreck Archive': Difference between revisions

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[https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802527.jp2&y=333&x=381 Link to the complete album]
[https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802527.jp2&y=333&x=381 Link to the complete album]


'''Notes:'''
== North Cornwall excursion, April, 1914 ==
 
'''The P number links are currently disabled.'''
 
'''Links to the album pages is work in progress in a Geologists' Association/British Geological Survey volunteer project.'''


{| class="wikitable"
{| class="wikitable"
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392551 P804235] || Crystals of orthoclase with inclusions of biotite in St. Austell Granite, Gready Quarry. North Cornwall, April 16th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802529.jp2&y=305&x=457 Page 3]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392551 P804235] || Crystals of orthoclase with inclusions of biotite in St. Austell Granite, Gready Quarry. North Cornwall, April 16th 1914.
|-
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802529.jp2&y=305&x=457 Page 3]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392552 P804236] || Crystals of orthoclase with inclusions of biotite in St. Austell Granite, Gready Quarry. North Cornwall, April 16th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392552 P804236] || Crystals of orthoclase with inclusions of biotite in St. Austell Granite, Gready Quarry. North Cornwall, April 16th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802529.jp2&y=305&x=457 Page 3]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392553 P804237] || Twinned crystal of orthoclase in St. Austell Granite, Gready Quarry. North Cornwall, April 16th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392553 P804237] || Twinned crystal of orthoclase in St. Austell Granite, Gready Quarry. North Cornwall, April 16th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802529.jp2&y=305&x=457 Page 3]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392554 P804238] || Luxulyanite. North Cornwall, April 16th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392554 P804238] || Luxulyanite. North Cornwall, April 16th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802531.jp2&y=305&x=459 Page 5]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392555 P804239] || Carpalla Pit. North Cornwall, April 17th 1914. Added note: Killas.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392555 P804239] || Carpalla Pit. North Cornwall, April 17th 1914. Added note: Killas.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802531.jp2&y=305&x=459 Page 5]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392556 P804240] || Carpalla Pit. North Cornwall, April 17th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392556 P804240] || Carpalla Pit. North Cornwall, April 17th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802531.jp2&y=305&x=459 Page 5]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392557 P804241] || Carpalla Pit. North Cornwall, April 17th 1914. Specimens of Killas from the above section.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392557 P804241] || Carpalla Pit. North Cornwall, April 17th 1914. Specimens of Killas from the above section.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802531.jp2&y=305&x=459 Page 5]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392558 P804242] || Carpalla Pit. North Cornwall, April 17th 1914. Specimens of Killas from the above section. Added note: Shewing tourmalined laminae (dark) alternating with arenaceous laminae (white) in which feldspar is Kaolinised.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392558 P804242] || Carpalla Pit. North Cornwall, April 17th 1914. Specimens of Killas from the above section. Added note: Shewing tourmalined laminae (dark) alternating with arenaceous laminae (white) in which feldspar is Kaolinised.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802533.jp2&y=305&x=461 Page 7]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392559 P804243] || Tregargus pit in China stone. North Cornwall, April 17th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392559 P804243] || Tregargus pit in China stone. North Cornwall, April 17th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802533.jp2&y=305&x=461 Page 7]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392560 P804244] || China stone with band of tourmaline. North Cornwall, April 17th 1914. Added note: Tourmaline.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392560 P804244] || China stone with band of tourmaline. North Cornwall, April 17th 1914. Added note: Tourmaline.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802533.jp2&y=305&x=461 Page 7]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392561 P804245] || Coarsely crystallised lithium bearing Biotite in pegmatite. Trelavour Downs. North Cornwall, April 17th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392561 P804245] || Coarsely crystallised lithium bearing Biotite in pegmatite. Trelavour Downs. North Cornwall, April 17th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802533.jp2&y=305&x=461 Page 7]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392562 P804246] || Coarsely crystallised lithium bearing biotite in pegmatite. Trelavour Downs. North Cornwall, April 17th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392562 P804246] || Coarsely crystallised lithium bearing biotite in pegmatite. Trelavour Downs. North Cornwall, April 17th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802535.jp2&y=305&x=463 Page 9]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392563 P804247] || Roche Rocks. North Cornwall, April 17th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392563 P804247] || Roche Rocks. North Cornwall, April 17th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802535.jp2&y=305&x=463 Page 9]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392564 P804248] || Roche Rocks. North Cornwall, April 17th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392564 P804248] || Roche Rocks. North Cornwall, April 17th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802535.jp2&y=305&x=463 Page 9]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392565 P804249] || Roche Rocks. North Cornwall, April 17th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392565 P804249] || Roche Rocks. North Cornwall, April 17th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802535.jp2&y=305&x=463 Page 9]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392566 P804250] || Roche Rocks. North Cornwall, April 17th 1914.  
|}
 
== Excursion to Derbyshire, July, 1914 ==
{| class="wikitable"
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392566 P804250] || Roche Rocks. North Cornwall, April 17th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802539.jp2&y=305&x=467 Page 13]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392567 P804251] || Black Rocks - Cromford. Millstone Grit Escarpment. Excursion to Derbyshire, July 28th 1914. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392567 P804251] || Black Rocks - Cromford. Millstone Grit Escarpment. Excursion to Derbyshire, July 28th 1914. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802539.jp2&y=305&x=467 Page 13]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392568 P804252] || Black Rocks - Cromford. Millstone Grit Escarpment. Excursion to Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392568 P804252] || Black Rocks - Cromford. Millstone Grit Escarpment. Excursion to Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802539.jp2&y=305&x=467 Page 13]
 
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392569 P804253] || In Derbyshire the Millstone Grit is made up of five thick beds of Sandstone each divided by a series of shales and sands interbedded. Excursion to Derbyshire, July 28th 1914. These 'Black Rocks' belong to the Fourth or Upper Kinder Scout Grit which here forms an escarpment. The rock standing out as bold craggy cliffs from the surrounding slopes and weathered into various shapes this having the fantastic title of the 'Field Gun'.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392569 P804253] || In Derbyshire the Millstone Grit is made up of five thick beds of Sandstone each divided by a series of shales and sands interbedded. Excursion to Derbyshire, July 28th 1914. These 'Black Rocks' belong to the Fourth or Upper Kinder Scout Grit which here forms an escarpment. The rock standing out as bold craggy cliffs from the surrounding slopes and weathered into various shapes this having the fantastic title of the 'Field Gun'.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802539.jp2&y=305&x=467 Page 13]
 
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392570 P804254] || In Derbyshire the Millstone Grit is made up of five thick beds of Sandstone each divided by a series of shales and sands interbedded. Excursion to Derbyshire, July 28th 1914. These 'Black Rocks' belong to the Fourth or Upper Kinder Scout Grit which here forms an escarpment. The rock standing out as bold craggy cliffs from the surrounding slopes and weathered into various shapes this having the fantastic title of the 'Field Gun'.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392570 P804254] || In Derbyshire the Millstone Grit is made up of five thick beds of Sandstone each divided by a series of shales and sands interbedded. Excursion to Derbyshire, July 28th 1914. These 'Black Rocks' belong to the Fourth or Upper Kinder Scout Grit which here forms an escarpment. The rock standing out as bold craggy cliffs from the surrounding slopes and weathered into various shapes this having the fantastic title of the 'Field Gun'.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802541.jp2&y=305&x=469 Page 15]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392571 P804255] || Dolomitized Mountain Limestone - Hopton Wood Quarry by Middleton. This stone was largely used in building the Imperial Institute. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392571 P804255] || Dolomitized Mountain Limestone - Hopton Wood Quarry by Middleton. This stone was largely used in building the Imperial Institute. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802541.jp2&y=305&x=469 Page 15]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392572 P804256] || Dolomitized Mountain Limestone - Hopton Wood Quarry by Middleton. This stone was largely used in building the Imperial Institute. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392572 P804256] || Dolomitized Mountain Limestone - Hopton Wood Quarry by Middleton. This stone was largely used in building the Imperial Institute. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802543.jp2&y=305&x=471 Page 17]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392573 P804257] || Section in the Dolerite Sill at Ible. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392573 P804257] || Section in the Dolerite Sill at Ible. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802543.jp2&y=305&x=471 Page 17]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392574 P804258] || [Ible]. Derbyshire, July 28th 1914. These igneous rocks of Derbyshire go by the name of Toadstones. Some say because the amydaloidal parts resemble the back of a toad while others trace it to the German word Todstein meaning dead stone because no ore is found in it.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392574 P804258] || [Ible]. Derbyshire, July 28th 1914. These igneous rocks of Derbyshire go by the name of Toadstones. Some say because the amydaloidal parts resemble the back of a toad while others trace it to the German word Todstein meaning dead stone because no ore is found in it.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802543.jp2&y=305&x=471 Page 17]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392575 P804259] || This sill at Ible is one of nine intrusions of igneous material in this part of Derbyshire. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392575 P804259] || This sill at Ible is one of nine intrusions of igneous material in this part of Derbyshire. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802543.jp2&y=305&x=471 Page 17]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392576 P804260] || [Ible]. Derbyshire, July 28th 1914. In the centre of the intrusion the dolerite is coarse grained and ophitic but at the margins it is very finegrained. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392576 P804260] || [Ible]. Derbyshire, July 28th 1914. In the centre of the intrusion the dolerite is coarse grained and ophitic but at the margins it is very finegrained. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802545.jp2&y=305&x=473 Page 19]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392577 P804261] || This sheet or sill of intrusive dolerite has a thickness of about 70 feet and is quarried for road metal. The Limestone below it has been baked into marble for a depth of several feet. Derbyshire, July 28th 1914. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392577 P804261] || This sheet or sill of intrusive dolerite has a thickness of about 70 feet and is quarried for road metal. The Limestone below it has been baked into marble for a depth of several feet. Derbyshire, July 28th 1914. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802545.jp2&y=305&x=473 Page 19]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392578 P804262] || This sheet or sill of intrusive dolerite has a thickness of about 70 feet and is quarried for road metal. The Limestone below it has been baked into marble for a depth of several feet. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392578 P804262] || This sheet or sill of intrusive dolerite has a thickness of about 70 feet and is quarried for road metal. The Limestone below it has been baked into marble for a depth of several feet. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802545.jp2&y=305&x=473 Page 19]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392579 P804263] || Joints in dolerite caused by shrinkage and disturbance. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392579 P804263] || Joints in dolerite caused by shrinkage and disturbance. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802545.jp2&y=305&x=473 Page 19]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392580 P804264] || Vein of Chrysolite in Dolerite Sill. Ible. Wirksworth. Derbyshire, July 28th 1914. These veins of chrysolite are found traversing the dolerite. The mineral is of a golden yellow colour and is built up of prisms or bundles of parallel fibres arranged perpendicularly to the walls of the cracks in which it has been deposited.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392580 P804264] || Vein of Chrysolite in Dolerite Sill. Ible. Wirksworth. Derbyshire, July 28th 1914. These veins of chrysolite are found traversing the dolerite. The mineral is of a golden yellow colour and is built up of prisms or bundles of parallel fibres arranged perpendicularly to the walls of the cracks in which it has been deposited.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802547.jp2&y=305&x=475 Page 21]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392581 P804265] || [Grange Mill]. Derbyshire, July 28th 1914. Shothouse Spring. nodular and concretionary limestone resting on a bed of laminated tuff. To a height of about 10 ft above the spring the limestone is found to contain numerous small lapilli.
|-| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802547.jp2&y=305&x=475 Page 21]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392582 P804266] || Grange Mill Vents. Derbyshire, July 28th 1914. These consist of two dome shaped hills which rise from the valley to a height of 100 and 200 ft. This larger one covers an area of 2400 to 1300 ft. The smooth and steep grassy slopes consist of a grey rock with green lapilli and limestone pebbles.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392581 P804265] || [Grange Mill]. Derbyshire, July 28th 1914. Shothouse Spring. nodular and concretionary limestone resting on a bed of laminated tuff. To a height of about 10 ft above the spring the limestone is found to contain numerous small lapilli.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802547.jp2&y=305&x=475 Page 21]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392583 P804267] || Agglomerate at Grange Mill which was formerly a volcanic vent. This weathers into spheroids as seen above which were exposed in the southern vent. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392582 P804266] || Grange Mill Vents. Derbyshire, July 28th 1914. These consist of two dome shaped hills which rise from the valley to a height of 100 and 200 ft. This larger one covers an area of 2400 to 1300 ft.  The smooth and steep grassy slopes consist of a grey rock with green lapilli and limestone pebbles.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802547.jp2&y=305&x=475 Page 21]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392584 P804268] || Agglomerate at Grange Mill which was formerly a volcanic vent. This weathers into spheroids as seen above which were exposed in the southern vent. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392583 P804267] || Agglomerate at Grange Mill which was formerly a volcanic vent. This weathers into spheroids as seen above which were exposed in the southern vent. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802549.jp2&y=305&x=477 Page 23]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392585 P804269] || Tufa Quarry, Via Gellia. This tufa consists of an amorphous carbonate of lime which has been deposited from a waterfall which previously existed at this place. Derbyshire, July 28th 1914. [Person].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392584 P804268] || Agglomerate at Grange Mill which was formerly a volcanic vent. This weathers into spheroids as seen above which were exposed in the southern vent. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802549.jp2&y=305&x=477 Page 23]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392586 P804270] || Tufa Quarry, Via Gellia. This tufa consists of an amorphous carbonate of lime which has been deposited from a waterfall which previously existed at this place. Derbyshire, July 28th 1914. [Person].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392585 P804269] || Tufa Quarry, Via Gellia. This tufa consists of an amorphous carbonate of lime which has been deposited from a waterfall which previously existed at this place. Derbyshire, July 28th 1914. [Person].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802549.jp2&y=305&x=477 Page 23]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392587 P804271] || [Via Gellia]. Derbyshire, July 28th 1914. The present stream and waterfall as now existing by the side of the quarry shown above.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392586 P804270] || Tufa Quarry, Via Gellia. This tufa consists of an amorphous carbonate of lime which has been deposited from a waterfall which previously existed at this place. Derbyshire, July 28th 1914. [Person].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802549.jp2&y=305&x=477 Page 23]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392588 P804272] || [Via Gellia]. Derbyshire, July 28th 1914. The present stream and waterfall as now existing by the side of the quarry shown above.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392587 P804271] || [Via Gellia]. Derbyshire, July 28th 1914. The present stream and waterfall as now existing by the side of the quarry shown above.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802551.jp2&y=305&x=479 Page 25]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392589 P804273] || Scrablag. A local name for peculiarly shaped concretions in sand. Ible. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392588 P804272] || [Via Gellia]. Derbyshire, July 28th 1914. The present stream and waterfall as now existing by the side of the quarry shown above.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802551.jp2&y=305&x=479 Page 25]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392590 P804274] || Scrablag. Ible Sill. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392589 P804273] || Scrablag. A local name for peculiarly shaped concretions in sand. Ible. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802551.jp2&y=305&x=479 Page 25]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392591 P804275] || Tufa. Via Gellia. Matlock Bath. Derbyshire, July 28th 1914. The Tufa is deposited around twigs, leaves, moss, shells, and bones of animals.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392590 P804274] || Scrablag. Ible Sill. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802551.jp2&y=305&x=479 Page 25]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392592 P804276] || Tufa. With Helix. Matlock Bath. Derbyshire, July 28th 1914. The Tufa is deposited around twigs, leaves, moss, shells, and bones of animals.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392591 P804275] || Tufa. Via Gellia. Matlock Bath. Derbyshire, July 28th 1914. The Tufa is deposited around twigs, leaves, moss, shells, and bones of animals.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802553.jp2&y=305&x=481 Page 27]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392593 P804277] || Carboniferous Limestone, Via Gellia. The smooth surface on the right is considered by some to be slickensided. Derbyshire, July 28th 1914. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392592 P804276] || Tufa. With Helix. Matlock Bath. Derbyshire, July 28th 1914. The Tufa is deposited around twigs, leaves, moss, shells, and bones of animals.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802553.jp2&y=305&x=481 Page 27]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392594 P804278] || Spheroidal dolerite, Via Gellia. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392593 P804277] || Carboniferous Limestone, Via Gellia. The smooth surface on the right is considered by some to be slickensided. Derbyshire, July 28th 1914. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802553.jp2&y=305&x=481 Page 27]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392595 P804279] || Quarry in spheroidal dolerite near the Paint Works, Via Gellia. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392594 P804278] || Spheroidal dolerite, Via Gellia. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802553.jp2&y=305&x=481 Page 27]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392596 P804280] || Quarry in spheroidal dolerite near the Paint Works, Via Gellia. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392595 P804279] || Quarry in spheroidal dolerite near the Paint Works, Via Gellia. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802555.jp2&y=305&x=483 Page 29]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392597 P804281] || Spheroidal dolerite in quarry near Pig of Lead, Matlock Bath. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392596 P804280] || Quarry in spheroidal dolerite near the Paint Works, Via Gellia. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802555.jp2&y=305&x=483 Page 29]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392598 P804282] || Spheroidal dolerite in quarry near Pig of Lead, Matlock Bath. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392597 P804281] || Spheroidal dolerite in quarry near Pig of Lead, Matlock Bath. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802555.jp2&y=305&x=483 Page 29]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392599 P804283] || Spheroidal dolerite in quarry near Pig of Lead, Matlock Bath. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392598 P804282] || Spheroidal dolerite in quarry near Pig of Lead, Matlock Bath. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802555.jp2&y=305&x=483 Page 29]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392600 P804284] || Spheroidal dolerite in quarry near Pig of Lead, Matlock Bath. Derbyshire, July 28th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392599 P804283] || Spheroidal dolerite in quarry near Pig of Lead, Matlock Bath. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802557.jp2&y=305&x=485 Page 31] || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392601 P804285] || Ravenstor, Millers Dale. Derbyshire, July 29th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392600 P804284] || Spheroidal dolerite in quarry near Pig of Lead, Matlock Bath. Derbyshire, July 28th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802557.jp2&y=305&x=485 Page 31]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392602 P804286] || Ravenstor, Millers Dale. Derbyshire, July 29th 1914. Carboniferous Limestone resting on Lower Lava.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392601 P804285] || Ravenstor, Millers Dale. Derbyshire, July 29th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802557.jp2&y=305&x=485 Page 31]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392603 P804287] || Ravenstor, Millers Dale. Derbyshire, July 29th 1914. In Tarnsley Dale. [Group photo].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392602 P804286] || Ravenstor, Millers Dale. Derbyshire, July 29th 1914. Carboniferous Limestone resting on Lower Lava.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802557.jp2&y=305&x=485 Page 31]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392604 P804288] || Ravenstor, Millers Dale. Derbyshire, July 29th 1914. Tideswell Dale.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392603 P804287] || Ravenstor, Millers Dale. Derbyshire, July 29th 1914. In Tarnsley Dale. [Group photo].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802559.jp2&y=305&x=487 Page 33]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392605 P804289] || Derbyshire, July 29th 1914. [Group photo, large version].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392604 P804288] || Ravenstor, Millers Dale. Derbyshire, July 29th 1914. Tideswell Dale.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802561.jp2&y=305&x=489 Page 35]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392606 P804290] || Derbyshire County Council Pit, Tideswell Dale. Derbyshire, July 29th 1914. This dolerite which is worked for road metal is found in a sill which has a thickness of about 70 feet. It extends for nearly half a mile in a North to South direction. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392605 P804289] || Derbyshire, July 29th 1914. [Group photo, large version].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802561.jp2&y=305&x=489 Page 35]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392607 P804291] || Derbyshire County Council Pit, Tideswell Dale. Derbyshire, July 29th 1914. The dolerite varies in structure, in the centre it is coarsely crystalline while at the upper and lower surfaces it is fine grained. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392606 P804290] || Derbyshire County Council Pit, Tideswell Dale. Derbyshire, July 29th 1914. This dolerite which is worked for road metal is found in a sill which has a thickness of about 70 feet. It extends for nearly half a mile in a North to South direction. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802561.jp2&y=305&x=489 Page 35]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392608 P804292] || Derbyshire County Council Pit, Tideswell Dale. Derbyshire, July 29th 1914. Spheroidal weathering.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392607 P804291] || Derbyshire County Council Pit, Tideswell Dale. Derbyshire, July 29th 1914. The dolerite varies in structure, in the centre it is coarsely crystalline while at the upper and lower surfaces it is fine grained. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802561.jp2&y=305&x=489 Page 35]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392609 P804293] || Derbyshire County Council Pit, Tideswell Dale. Derbyshire, July 29th 1914. Spheroidal weathering.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392608 P804292] || Derbyshire County Council Pit, Tideswell Dale. Derbyshire, July 29th 1914. Spheroidal weathering.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802563.jp2&y=305&x=491 Page 37]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392610 P804294] || Columnar Volcanic Mud. Baked by Lava Flow. Tideswell Dale. Derbyshire, July 29th 1914. At Tideswell Dale is a bed of red clay which was formerly a volcanic mud. This is found interbedded in the limestone. After its deposition a stream of lava flowed over it which hardened and baked it and caused it to assume a columnar structure.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392609 P804293] || Derbyshire County Council Pit, Tideswell Dale. Derbyshire, July 29th 1914. Spheroidal weathering.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802563.jp2&y=305&x=491 Page 37]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392611 P804295] || Columnar Volcanic Mud. Baked by Lava Flow. Tideswell Dale. Derbyshire, July 29th 1914. At Tideswell Dale is a bed of red clay which was formerly a volcanic mud. This is found interbedded in the limestone. After its deposition a stream of lava flowed over it which hardened and baked it and caused it to assume a columnar structure.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392610 P804294] || Columnar Volcanic Mud. Baked by Lava Flow. Tideswell Dale. Derbyshire, July 29th 1914. At Tideswell Dale is a bed of red clay which was formerly a volcanic mud. This is found interbedded in the limestone. After its deposition a stream of lava flowed over it which hardened and baked it and caused it to assume a columnar structure.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802563.jp2&y=305&x=491 Page 37]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392612 P804296] || Carboniferous limestone, Monsal Dale. Derbyshire, July 29th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392611 P804295] || Columnar Volcanic Mud. Baked by Lava Flow. Tideswell Dale. Derbyshire, July 29th 1914. At Tideswell Dale is a bed of red clay which was formerly a volcanic mud. This is found interbedded in the limestone. After its deposition a stream of lava flowed over it which hardened and baked it and caused it to assume a columnar structure.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802563.jp2&y=305&x=491 Page 37]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392613 P804297] || Spheroides of Dolerite. Tideswell Dale. Derbyshire, July 29th 1914. Owing to a chemical change in the dolerite due to weathering the blocks assume a spheroidal form.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392612 P804296] || Carboniferous limestone, Monsal Dale. Derbyshire, July 29th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802565.jp2&y=305&x=493 Page 39]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392614 P804298] || Peep o' Day Quarry in the Carboniferous Limestone at Litton. This was originally a coral reef but is now consolidated into a hard massive limestone. Derbyshire, July 29th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392613 P804297] || Spheroides of Dolerite. Tideswell Dale. Derbyshire, July 29th 1914. Owing to a chemical change in the dolerite due to weathering the blocks assume a spheroidal form.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802565.jp2&y=305&x=493 Page 39]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392615 P804299] || Peep o' Day Quarry in the Carboniferous Limestone at Litton. This was originally a coral reef but is now consolidated into a hard massive limestone. Derbyshire, July 29th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392614 P804298] || Peep o' Day Quarry in the Carboniferous Limestone at Litton. This was originally a coral reef but is now consolidated into a hard massive limestone. Derbyshire, July 29th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802565.jp2&y=305&x=493 Page 39]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392616 P804300] || [Peep o' Day Quary]. Derbyshire, July 29th 1914. Owing to the action of the weather on the exposed surfaces of the limestones the fine coral mud is gradually worn away leaving the corals standing out in relief in the positions in which they lived. Added note: coral.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392615 P804299] || Peep o' Day Quarry in the Carboniferous Limestone at Litton. This was originally a coral reef but is now consolidated into a hard massive limestone. Derbyshire, July 29th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802565.jp2&y=305&x=493 Page 39]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392617 P804301] || [Peep o' Day Quary]. Derbyshire, July 29th 1914. Owing to the action of the weather on the exposed surfaces of the limestones the fine coral mud is gradually worn away leaving the corals standing out in relief in the positions in which they lived. Added note: coral.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392616 P804300] || [Peep o' Day Quary]. Derbyshire, July 29th 1914. Owing to the action of the weather on the exposed surfaces of the limestones the fine coral mud is gradually worn away leaving the corals standing out in relief in the positions in which they lived. Added note: coral.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802567.jp2&y=305&x=495 Page 41]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392618 P804302] || Stepping stones across bed of what is a mountain torrent after rain. Cressbrook Dale. Derbyshire, July 29th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392617 P804301] || [Peep o' Day Quary]. Derbyshire, July 29th 1914. Owing to the action of the weather on the exposed surfaces of the limestones the fine coral mud is gradually worn away leaving the corals standing out in relief in the positions in which they lived. Added note: coral.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802567.jp2&y=305&x=495 Page 41]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392619 P804303] || [Cressbrook Dale]. Derbyshire, July 29th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392618 P804302] || Stepping stones across bed of what is a mountain torrent after rain. Cressbrook Dale. Derbyshire, July 29th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802567.jp2&y=305&x=495 Page 41]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392620 P804304] || [Cressbrook Dale]. Derbyshire, July 29th 1914. Cressbrook Mill Stream! In dry weather this is a dry river bed in the Carboniferous limestone but after rain it becomes a mountain torrent. It shows the angular blocks being formed into pebbles.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392619 P804303] || [Cressbrook Dale]. Derbyshire, July 29th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802567.jp2&y=305&x=495 Page 41]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392621 P804305] || [Cressbrook Dale]. Derbyshire, July 29th 1914. Cressbrook Mill Stream! In dry weather this is a dry river bed in the Carboniferous limestone but after rain it becomes a mountain torrent. It shows the angular blocks being formed into pebbles.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392620 P804304] || [Cressbrook Dale]. Derbyshire, July 29th 1914. Cressbrook Mill Stream! In dry weather this is a dry river bed in the Carboniferous limestone but after rain it becomes a mountain torrent. It shows the angular blocks being formed into pebbles.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802569.jp2&y=305&x=497 Page 43]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392622 P804306] || Derbyshire, July 29th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392621 P804305] || [Cressbrook Dale]. Derbyshire, July 29th 1914. Cressbrook Mill Stream! In dry weather this is a dry river bed in the Carboniferous limestone but after rain it becomes a mountain torrent. It shows the angular blocks being formed into pebbles.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802569.jp2&y=305&x=497 Page 43]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392623 P804307] || Derbyshire, July 29th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392622 P804306] || Derbyshire, July 29th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802569.jp2&y=305&x=497 Page 43]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392624 P804308] || River Wye at Monsal Dale (Headstones). Derbyshire, July 29th 1914. The River Wye generally described as 'a singularly romantic river, running in deep rocky ravines, its clear stream sparkling along a confined and rugged bed' rises near Buxton on the northern slope of Axe Edge and joins the Derwent at Rowsley.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392623 P804307] || Derbyshire, July 29th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802569.jp2&y=305&x=497 Page 43]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392625 P804309] || River Wye at Monsal Dale (Headstones). Derbyshire, July 29th 1914. The River Wye generally described as 'a singularly romantic river, running in deep rocky ravines, its clear stream sparkling along a confined and rugged bed' rises near Buxton on the northern slope of Axe Edge and joins the Derwent at Rowsley.
|-
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392624 P804308] || River Wye at Monsal Dale (Headstones). Derbyshire, July 29th 1914. The River Wye generally described as 'a singularly romantic river, running in deep rocky ravines, its clear stream sparkling along a confined and rugged bed' rises near Buxton on the northern slope of Axe Edge and joins the Derwent at Rowsley.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802571.jp2&y=305&x=499 Page 45]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392626 P804310] || Boulder Clay overlying Carboniferous Limestone, Monsal Dale Station Quarry. Derbyshire, July 29th 1914. Some of the boulders consist of rock derived from the immediate locality while others have travelled from great distances, they are much scratched grooved and polished.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392625 P804309] || River Wye at Monsal Dale (Headstones). Derbyshire, July 29th 1914. The River Wye generally described as 'a singularly romantic river, running in deep rocky ravines, its clear stream sparkling along a confined and rugged bed' rises near Buxton on the northern slope of Axe Edge and joins the Derwent at Rowsley.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802571.jp2&y=305&x=499 Page 45]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392627 P804311] || Boulder Clay overlying Carboniferous Limestone, Monsal Dale Station Quarry. Derbyshire, July 29th 1914. Some of the boulders consist of rock derived from the immediate locality while others have travelled from great distances, they are much scratched grooved and polished. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392626 P804310] || Boulder Clay overlying Carboniferous Limestone, Monsal Dale Station Quarry. Derbyshire, July 29th 1914. Some of the boulders consist of rock derived from the immediate locality while others have travelled from great distances, they are much scratched grooved and polished.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802571.jp2&y=305&x=499 Page 45]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392628 P804312] || Slickensided Carboniferous Limestone caused by one face of the rock sliding over the other owing to earth movements. Derbyshire, July 29th 1914.  
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392627 P804311] || Boulder Clay overlying Carboniferous Limestone, Monsal Dale Station Quarry. Derbyshire, July 29th 1914. Some of the boulders consist of rock derived from the immediate locality while others have travelled from great distances, they are much scratched grooved and polished. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802571.jp2&y=305&x=499 Page 45]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392629 P804313] || Calc spar mine, Monsal Dale. This mine for obtaining calc spar is driven into a rake vein about 2 feet in width in the Carboniferous limestone. The vein is filled with calc spar with galena and barytes. Derbyshire, July 29th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392628 P804312] || Slickensided Carboniferous Limestone caused by one face of the rock sliding over the other owing to earth movements. Derbyshire, July 29th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802573.jp2&y=305&x=501 Page 47]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392630 P804314] || Ridgeway Cutting, Ambergate. Derbyshire, July 30th 1914. Overthrust Fault in Coal seam, locally known as the 'Norton' seam.
|-
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392629 P804313] || Calc spar mine, Monsal Dale. This mine for obtaining calc spar is driven into a rake vein about 2 feet in width in the Carboniferous limestone. The vein is filled with calc spar with galena and barytes. Derbyshire, July 29th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802573.jp2&y=305&x=501 Page 47]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392631 P804315] || Ridgeway Cutting, Ambergate. Derbyshire, July 30th 1914. Lower Coal Measures, Ridgeway Ry [Railway] Cutting.
|-
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392630 P804314] || Ridgeway Cutting, Ambergate. Derbyshire, July 30th 1914. Overthrust Fault in Coal seam, locally known as the 'Norton' seam.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802573.jp2&y=305&x=501 Page 47] || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392632 P804316] || Ridgeway Cutting, Ambergate. Derbyshire, July 30th 1914. Coal seam, 'Norton' Seam. [Person].
|-
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392631 P804315] || Ridgeway Cutting, Ambergate. Derbyshire, July 30th 1914. Lower Coal Measures, Ridgeway Ry [Railway] Cutting.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802573.jp2&y=305&x=501 Page 47]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392633 P804317] || Ridgeway Cutting, Ambergate. Derbyshire, July 30th 1914. Lower Coal Measures in Ridgeway Cutting. Added note: 4=shales, 3=Gannister, 2=White Snady Fine Clay, 1=Sandstone.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392632 P804316] || Ridgeway Cutting, Ambergate. Derbyshire, July 30th 1914. Coal seam, 'Norton' Seam. [Person].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802575.jp2&y=305&x=503 Page 49]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392634 P804318] || Ridgeway Quarry in Millstone Grit. The Topmost Grit or 'Rough Rock'. Derbyshire, July 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392633 P804317] || Ridgeway Cutting, Ambergate. Derbyshire, July 30th 1914. Lower Coal Measures in Ridgeway Cutting. Added note: 4=shales, 3=Gannister, 2=White Snady Fine Clay, 1=Sandstone.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802575.jp2&y=305&x=503 Page 49]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392635 P804319] || Bullbridge Brickyard Pit in the Lower Coal Measures. Derbyshire, July 30th 1914. Added note: Shale resting on Marine Band above Alton Seam.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392634 P804318] || Ridgeway Quarry in Millstone Grit. The Topmost Grit or 'Rough Rock'. Derbyshire, July 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802575.jp2&y=305&x=503 Page 49]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392636 P804320] || The Alton Coal seam Bullbridge Brickyard. This coal seam is about 300 feet above the base of the Coal Measures and is correlated with the Crabtree Coal of North Staffordshire and the Bullion Coal of Lancashire. Derbyshire, July 30th 1914. [Person].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392635 P804319] || Bullbridge Brickyard Pit in the Lower Coal Measures. Derbyshire, July 30th 1914. Added note: Shale resting on Marine Band above Alton Seam.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802575.jp2&y=305&x=503 Page 49]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392637 P804321] || The Alton Coal seam Bullbridge Brickyard. This coal seam is about 300 feet above the base of the Coal Measures and is correlated with the Crabtree Coal of North Staffordshire and the Bullion Coal of Lancashire. Derbyshire, July 30th 1914. [Person].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392636 P804320] || The Alton Coal seam Bullbridge Brickyard. This coal seam is about 300 feet above the base of the Coal Measures and is correlated with the Crabtree Coal of North Staffordshire and the Bullion Coal of Lancashire. Derbyshire, July 30th 1914. [Person].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802577.jp2&y=305&x=505 Page 51]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392638 P804322] || Crich. Derbyshire, July 30th 1914. This inlier consists of a mass of Carboniferous Limestone about 1.5 miles in length. It forms an elongated dome running from N.N.W. to S.S.E.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392637 P804321] || The Alton Coal seam Bullbridge Brickyard. This coal seam is about 300 feet above the base of the Coal Measures and is correlated with the Crabtree Coal of North Staffordshire and the Bullion Coal of Lancashire. Derbyshire, July 30th 1914. [Person].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802577.jp2&y=305&x=505 Page 51]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392639 P804323] || Crich. Derbyshire, July 30th 1914. This tower known as Crich Stand is built on the summit of a mass of Carboniferous Limestone known as the Crich inlier. It is 940 feet above sea level.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392638 P804322] || Crich. Derbyshire, July 30th 1914. This inlier consists of a mass of Carboniferous Limestone about 1.5 miles in length. It forms an elongated dome running from N.N.W. to S.S.E.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802577.jp2&y=305&x=505 Page 51]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392640 P804324] || Crich. Derbyshire, July 30th 1914. Mammilated surface of Limestone. Cliff Quarry, Crich.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392639 P804323] || Crich. Derbyshire, July 30th 1914. This tower known as Crich Stand is built on the summit of a mass of Carboniferous Limestone known as the Crich inlier. It is 940 feet above sea level.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802577.jp2&y=305&x=505 Page 51]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392641 P804325] || Crich. Derbyshire, July 30th 1914. Cliff Quarry in the Crich inlier Carb. [Carboniferous] Limestone. This is D2. of Dr Vaughan. The limestone is traversed with viens containing Calcite, Fluorite, barytes, galena and Blendes. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392640 P804324] || Crich. Derbyshire, July 30th 1914. Mammilated surface of Limestone. Cliff Quarry, Crich.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802579.jp2&y=305&x=507 Page 53]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392642 P804326] || The Old Quarry in Carboniferous Limestone, Crich. The Limestone is capped by Glacial Drift containing local and foreign erratics. Derbyshire, July 30th 1914.  
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|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392641 P804325] || Crich. Derbyshire, July 30th 1914. Cliff Quarry in the Crich inlier Carb. [Carboniferous] Limestone. This is D2. of Dr Vaughan. The limestone is traversed with viens containing Calcite, Fluorite, barytes, galena and Blendes. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802579.jp2&y=305&x=507 Page 53]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392643 P804327] || The Old Quarry in Carboniferous Limestone, Crich. The Limestone is capped by Glacial Drift containing local and foreign erratics. Derbyshire, July 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392642 P804326] || The Old Quarry in Carboniferous Limestone, Crich. The Limestone is capped by Glacial Drift containing local and foreign erratics. Derbyshire, July 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802579.jp2&y=305&x=507 Page 53]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392644 P804328] || [Old Quarry, Crich]. Derbyshire, July 30th 1914. 'Pothole'. Solution-cavities in limestone filled with clay.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392643 P804327] || The Old Quarry in Carboniferous Limestone, Crich. The Limestone is capped by Glacial Drift containing local and foreign erratics. Derbyshire, July 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802579.jp2&y=305&x=507 Page 53]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392645 P804329] || The Old Quarry, Crich. Solution cavities in Carb. [Carboniferous] Limestone filled with clay. Derbyshire, July 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392644 P804328] || [Old Quarry, Crich]. Derbyshire, July 30th 1914. 'Pothole'. Solution-cavities in limestone filled with clay.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802581.jp2&y=305&x=509 Page 55]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392646 P804330] || Hilt's Quarry, Crich. Carboniferous Limestone. Derbyshire, July 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392645 P804329] || The Old Quarry, Crich. Solution cavities in Carb. [Carboniferous] Limestone filled with clay. Derbyshire, July 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802581.jp2&y=305&x=509 Page 55]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392647 P804331] || Hilt's Quarry, Crich. Carboniferous Limestone. Derbyshire, July 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392646 P804330] || Hilt's Quarry, Crich. Carboniferous Limestone. Derbyshire, July 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802583.jp2&y=305&x=511 Page 57]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392648 P804332] || Howden Dam. Derbyshire, July 31st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392647 P804331] || Hilt's Quarry, Crich. Carboniferous Limestone. Derbyshire, July 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802583.jp2&y=305&x=511 Page 57]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392649 P804333] || Anticline in shales and sandstones on river bank below Howden Dam. Derbyshire, July 31st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392648 P804332] || Howden Dam. Derbyshire, July 31st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802583.jp2&y=305&x=511 Page 57]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392650 P804334] || Anticline in shales and sandstones on river bank below Howden Dam. Derbyshire, July 31st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392649 P804333] || Anticline in shales and sandstones on river bank below Howden Dam. Derbyshire, July 31st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802585.jp2&y=305&x=513 Page 59]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392651 P804335] || Darley Dale Quarry. Derbyshire, August 1st 1914. The Mountain Limestone forms in Derbyshire an inlier of an irregular shape stretching 20 miles from North to South and above 10 miles from East to West with a few little patches in other localities. Owing to earth movements this large inlier forms a pericline or dome, the beds dipping away from the middle of the dome in every direction.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392650 P804334] || Anticline in shales and sandstones on river bank below Howden Dam. Derbyshire, July 31st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802585.jp2&y=305&x=513 Page 59]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392652 P804336] || Darley Dale Quarry. Derbyshire, August 1st 1914. The Mountain Limestone forms in Derbyshire an inlier of an irregular shape stretching 20 miles from North to South and above 10 miles from East to West with a few little patches in other localities. Owing to earth movements this large inlier forms a pericline or dome, the beds dipping away from the middle of the dome in every direction.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392651 P804335] || Darley Dale Quarry. Derbyshire, August 1st 1914. The Mountain Limestone forms in Derbyshire an inlier of an irregular shape stretching 20 miles from North to South and above 10 miles from East to West with a few little patches in other localities. Owing to earth movements this large inlier forms a pericline or dome, the beds dipping away from the middle of the dome in every direction.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802585.jp2&y=305&x=513 Page 59]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392653 P804337] || Darley Dale Quarry. Derbyshire, August 1st 1914. On examination it appears that some of the layers had their origin from reef like accumulations very much like those in the Pacific coral islands and shell banks while others were more fragmental and made up of broken corals, crinoid stems and shells which the waves had spread over the sea bottom.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392652 P804336] || Darley Dale Quarry. Derbyshire, August 1st 1914. The Mountain Limestone forms in Derbyshire an inlier of an irregular shape stretching 20 miles from North to South and above 10 miles from East to West with a few little patches in other localities. Owing to earth movements this large inlier forms a pericline or dome, the beds dipping away from the middle of the dome in every direction.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802585.jp2&y=305&x=513 Page 59]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392654 P804338] || Darley Dale Quarry. Derbyshire, August 1st 1914. On examination it appears that some of the layers had their origin from reef like accumulations very much like those in the Pacific coral islands and shell banks while others were more fragmental and made up of broken corals, crinoid stems and shells which the waves had spread over the sea bottom. Added note: Crinoidal limestone beds.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392653 P804337] || Darley Dale Quarry. Derbyshire, August 1st 1914. On examination it appears that some of the layers had their origin from reef like accumulations very much like those in the Pacific coral islands and shell banks while others were more fragmental and made up of broken corals, crinoid stems and shells which the waves had spread over the sea bottom.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802587.jp2&y=305&x=515 Page 61]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392655 P804339] || Dolomitized limestone or Dunstone showing the typical weathering into castellated masses at Wyn's Tor above Winster. Derbyshire, August 1st 1914. [Group photo].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392654 P804338] || Darley Dale Quarry. Derbyshire, August 1st 1914. On examination it appears that some of the layers had their origin from reef like accumulations very much like those in the Pacific coral islands and shell banks while others were more fragmental and made up of broken corals, crinoid stems and shells which the waves had spread over the sea bottom. Added note: Crinoidal limestone beds.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802587.jp2&y=305&x=515 Page 61]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392656 P804340] || Dolomitized limestone or Dunstone showing the typical weathering into castellated masses at Wyn's Tor above Winster. Derbyshire, August 1st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392655 P804339] || Dolomitized limestone or Dunstone showing the typical weathering into castellated masses at Wyn's Tor above Winster. Derbyshire, August 1st 1914. [Group photo].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802587.jp2&y=305&x=515 Page 61]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392657 P804341] || Chert quarry, Winster. Derbyshire, August 1st 1914. This chert is a silicious limestone which is sent to the Staffordshire potteries for making china and porcelain. Owing to its crystalline structure it differs from the nodules and layers of chert which are found in the upper beds of the Mountain limestone. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392656 P804340] || Dolomitized limestone or Dunstone showing the typical weathering into castellated masses at Wyn's Tor above Winster. Derbyshire, August 1st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802587.jp2&y=305&x=515 Page 61]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392658 P804342] || Chert quarry, Winster. Derbyshire, August 1st 1914. This chert is a silicious limestone which is sent to the Staffordshire potteries for making china and porcelain. Owing to its crystalline structure it differs from the nodules and layers of chert which are found in the upper beds of the Mountain limestone. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392657 P804341] || Chert quarry, Winster. Derbyshire, August 1st 1914. This chert is a silicious limestone which is sent to the Staffordshire potteries for making china and porcelain. Owing to its crystalline structure it differs from the nodules and layers of chert which are found in the upper beds of the Mountain limestone. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802589.jp2&y=305&x=517 Page 63]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392659 P804343] || Robin Hoods Stride or Mock Beggars Hall in the Fourth or Upper Kinder Scout Grit of the Millstone Grit. Derbyshire, August 1st 1914. The stride which Robin Hood must have taken to get the place named after him, that is, the distance from these two turrets is about 10 to 15 yards. [People].
|-
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392658 P804342] || Chert quarry, Winster. Derbyshire, August 1st 1914. This chert is a silicious limestone which is sent to the Staffordshire potteries for making china and porcelain. Owing to its crystalline structure it differs from the nodules and layers of chert which are found in the upper beds of the Mountain limestone. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802589.jp2&y=305&x=517 Page 63]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392660 P804344] || Robin Hoods Stride or Mock Beggars Hall in the Fourth or Upper Kinder Scout Grit of the Millstone Grit. Derbyshire, August 1st 1914. The stride which Robin Hood must have taken to get the place named after him, that is, the distance from these two turrets is about 10 to 15 yards. [People].
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|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392659 P804343] || Robin Hoods Stride or Mock Beggars Hall in the Fourth or Upper Kinder Scout Grit of the Millstone Grit. Derbyshire, August 1st 1914. The stride which Robin Hood must have taken to get the place named after him, that is, the distance from these two turrets is about 10 to 15 yards. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802589.jp2&y=305&x=517 Page 63]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392661 P804345] || Cone-In-Cone. Bullbridge Ambergate. Derbyshire, August 1st 1914.  
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|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392660 P804344] || Robin Hoods Stride or Mock Beggars Hall in the Fourth or Upper Kinder Scout Grit of the Millstone Grit. Derbyshire, August 1st 1914. The stride which Robin Hood must have taken to get the place named after him, that is, the distance from these two turrets is about 10 to 15 yards. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802591.jp2&y=305&x=519 Page 65]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392662 P804346] || The Dakin Valley, Alport, showing the thick horizontal beds of Carboniferous limestone. It is from these 'Scars' which are bare precipices or mural escarpments that Sedgwick named this the 'Scar limestone'. Derbyshire, August 1st 1914. [People].
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392661 P804345] || Cone-In-Cone. Bullbridge Ambergate. Derbyshire, August 1st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802591.jp2&y=305&x=519 Page 65]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392663 P804347] || The Dakin Valley, Alport, showing the thick horizontal beds of Carboniferous limestone. It is from these 'Scars' which are bare precipices or mural escarpments that Sedgwick named this the 'Scar Limestone'. Derbyshire, August 1st 1914.  
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392662 P804346] || The Dakin Valley, Alport, showing the thick horizontal beds of Carboniferous limestone. It is from these 'Scars' which are bare precipices or mural escarpments that Sedgwick named this the 'Scar limestone'. Derbyshire, August 1st 1914. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802591.jp2&y=305&x=519 Page 65]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392664 P804348] || [Joints]. Derbyshire, August 1st 1914. In these scars are frequently seen joints like the above which are formed by shrinkage and sometimes by disturbance. These cracks which are generally at right angles to the bedding are gradually enlanged by the action of water.
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392663 P804347] || The Dakin Valley, Alport, showing the thick horizontal beds of Carboniferous limestone. It is from these 'Scars' which are bare precipices or mural escarpments that Sedgwick named this the 'Scar Limestone'. Derbyshire, August 1st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802591.jp2&y=305&x=519 Page 65]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392665 P804349] || Tufa Quarry, Alport. This creamy white rock is formed by the deposition of lime from calcareous springs and is of variable texture, in places being hard and crystalline and in others soft, friable and cellular. Derbyshire, August 1st 1914. [Person].
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392664 P804348] || [Joints]. Derbyshire, August 1st 1914. In these scars are frequently seen joints like the above which are formed by shrinkage and sometimes by disturbance. These cracks which are generally at right angles to the bedding are gradually enlanged by the action of water.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802593.jp2&y=305&x=521 Page 67]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392666 P804350] || Old Mill Quarry,Stanton Mill. The Black Shales of the Pendleside Series containing Posidoniella laevis are here seen to rest with unconformity on the limestones of the Lonsdalia subzone. Derbyshire, August 1st 1914. The shales which show no signs of disturbance rest evenly upon a surface formed by the truncated edges of the limestone beds. This shows the commencement of an anticlinal dome of limestone. If stripped of the shale above, the dome would have a knoll like aspect thus indicating contemporaneous elevation and erosion causing local unconformity. Added note: Grey limestones with strong chert, Carboniferous Limestone, Lonsdalia sub-zone. Black Shales, Pendleside Series.
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392665 P804349] || Tufa Quarry, Alport. This creamy white rock is formed by the deposition of lime from calcareous springs and is of variable texture, in places being hard and crystalline and in others soft, friable and cellular. Derbyshire, August 1st 1914. [Person].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802593.jp2&y=305&x=521 Page 67]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392667 P804351] || Old Mill Quarry,Stanton Mill. The Black Shales of the Pendleside Series containing Posidoniella laevis are here seen to rest with unconformity on the Limestones of the Lonsdalia subzone. Derbyshire, August 1st 1914. The shales which show no signs of disturbance rest evenly upon a surface formed by the truncated edges of the limestone beds. This shows the commencement of an anticlinal dome of Limestone. If stripped of the shale above, the dome would have a knoll like aspect thus indicating contemporaneous elevation and erosion causing local unconformity. Added note: Limestone, Black Shales. [People].
|-
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392666 P804350] || Old Mill Quarry,Stanton Mill. The Black Shales of the Pendleside Series containing Posidoniella laevis are here seen to rest with unconformity on the limestones of the Lonsdalia subzone. Derbyshire, August 1st 1914. The shales which show no signs of disturbance rest evenly upon a surface formed by the truncated edges of the limestone beds. This shows the commencement of an anticlinal dome of limestone. If stripped of the shale above, the dome would have a knoll like aspect thus indicating contemporaneous elevation and erosion causing local unconformity. Added note: Grey limestones with strong chert, Carboniferous Limestone, Lonsdalia sub-zone. Black Shales, Pendleside Series.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802593.jp2&y=305&x=521 Page 67]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392668 P804352] || Old Mill Quarry,Stanton Mill. The Black Shales of the Pendleside Series containing Posidoniella laevis are here seen to rest with unconformity on the Limestones of the Lonsdalia subzone. Derbyshire, August 1st 1914. The shales which show no signs of disturbance rest evenly upon a surface formed by the truncated edges of the limestone beds. This shows the commencement of an anticlinal dome of Limestone. If stripped of the shale above, the dome would have a knoll like aspect thus indicating contemporaneous elevation and erosion causing local unconformity.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392667 P804351] || Old Mill Quarry,Stanton Mill. The Black Shales of the Pendleside Series containing Posidoniella laevis are here seen to rest with unconformity on the Limestones of the Lonsdalia subzone. Derbyshire, August 1st 1914. The shales which show no signs of disturbance rest evenly upon a surface formed by the truncated edges of the limestone beds. This shows the commencement of an anticlinal dome of Limestone. If stripped of the shale above, the dome would have a knoll like aspect thus indicating contemporaneous elevation and erosion causing local unconformity. Added note: Limestone, Black Shales. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802593.jp2&y=305&x=521 Page 67]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392669 P804353] || River Dakin - Alport. This is an interesting case of a calcareous stream forming terraces of travertine or tufa. The calcium carbonate being thrown down in ridges or terraces by the escape of carbonic acid and evaporation. Derbyshire, August 1st 1914.  
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392668 P804352] || Old Mill Quarry,Stanton Mill. The Black Shales of the Pendleside Series containing Posidoniella laevis are here seen to rest with unconformity on the Limestones of the Lonsdalia subzone. Derbyshire, August 1st 1914. The shales which show no signs of disturbance rest evenly upon a surface formed by the truncated edges of the limestone beds. This shows the commencement of an anticlinal dome of Limestone. If stripped of the shale above, the dome would have a knoll like aspect thus indicating contemporaneous elevation and erosion causing local unconformity.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802595.jp2&y=305&x=523 Page 69]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392670 P804354] || Harboro' [Harborough] pit, Brassington. Derbyshire, August 2nd 1914. These deposits of brightly coloured sands and clays in various shades of red and yellow with white are found in large irregular hollows in the Carboniferous Limestone occurring between Hartington and Brassington in a N.W. to S.E. direction. These hollows which are sometimes 100 yards across are thought to be swallow holes filled in with fine clay and clean sand with white and red quartzite pebbles. Their age is uncertain - they are evidently preglacial and some go so far as to consider them of Bunter age. The materials have the character of a broken up Kinder Scout Grit and the sands and pebbles agree with the Bunter Beds. The clay obtained here is used by the Derby Porcelain works. [Caption of two photos combined as form continuous text].
|-
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392669 P804353] || River Dakin - Alport. This is an interesting case of a calcareous stream forming terraces of travertine or tufa. The calcium carbonate being thrown down in ridges or terraces by the escape of carbonic acid and evaporation. Derbyshire, August 1st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802595.jp2&y=305&x=523 Page 69]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392671 P804355] || Harboro' [Harborough] pit, Brassington. Derbyshire, August 2nd 1914. These deposits of brightly coloured sands and clays in various shades of red and yellow with white are found in large irregular hollows in the Carboniferous Limestone occurring between Hartington and Brassington in a N.W. to S.E. direction. These hollows which are sometimes 100 yards across are thought to be swallow holes filled in with fine clay and clean sand with white and red quartzite pebbles. Their age is uncertain - they are evidently preglacial and some go so far as to consider them of Bunter age. The materials have the character of a broken up Kinder Scout Grit and the sands and pebbles agree with the Bunter Beds. The clay obtained here is used by the Derby Porcelain works. [Caption of two photos combined as form continuous text].
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392670 P804354] || Harboro' [Harborough] pit, Brassington. Derbyshire, August 2nd 1914. These deposits of brightly coloured sands and clays in various shades of red and yellow with white are found in large irregular hollows in the Carboniferous Limestone occurring between Hartington and Brassington in a N.W. to S.E. direction. These hollows which are sometimes 100 yards across are thought to be swallow holes filled in with fine clay and clean sand with white and red quartzite pebbles. Their age is uncertain - they are evidently preglacial and some go so far as to consider them of Bunter age. The materials have the character of a broken up Kinder Scout Grit and the sands and pebbles agree with the Bunter Beds. The clay obtained here is used by the Derby Porcelain works. [Caption of two photos combined as form continuous text].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802597.jp2&y=305&x=525 Page 71]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392672 P804356] || Carboniferous Limestone, Cromford. Derbyshire, August 3rd 1914.  
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392671 P804355] || Harboro' [Harborough] pit, Brassington. Derbyshire, August 2nd 1914. These deposits of brightly coloured sands and clays in various shades of red and yellow with white are found in large irregular hollows in the Carboniferous Limestone occurring between Hartington and Brassington in a N.W. to S.E. direction. These hollows which are sometimes 100 yards across are thought to be swallow holes filled in with fine clay and clean sand with white and red quartzite pebbles. Their age is uncertain - they are evidently preglacial and some go so far as to consider them of Bunter age. The materials have the character of a broken up Kinder Scout Grit and the sands and pebbles agree with the Bunter Beds. The clay obtained here is used by the Derby Porcelain works. [Caption of two photos combined as form continuous text].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802597.jp2&y=305&x=525 Page 71]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392673 P804357] || Cromford Quarry. Derbyshire, August 3rd 1914. [Person].
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392672 P804356] || Carboniferous Limestone, Cromford. Derbyshire, August 3rd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802597.jp2&y=305&x=525 Page 71]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392674 P804358] || Bonsall. Derbyshire, August 3rd 1914. [Group photo].
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392673 P804357] || Cromford Quarry. Derbyshire, August 3rd 1914. [Person].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802597.jp2&y=305&x=525 Page 71]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392675 P804359] || Quartzose Limestone, Bonsall. Derbyshire, August 3rd 1914.  
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392674 P804358] || Bonsall. Derbyshire, August 3rd 1914. [Group photo].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802599.jp2&y=305&x=527 Page 73]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392676 P804360] || [Bonsall]. Derbyshire, August 3rd 1914. [Group photo - large version of previous].
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392675 P804359] || Quartzose Limestone, Bonsall. Derbyshire, August 3rd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802601.jp2&y=305&x=529 Page 75]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392677 P804361] || Quarry in Spheroidal Dolerite - Pot Luck Farm (Drabble's Quarry), Bonsall. Derbyshire, August 3rd 1914. When the Carboniferous limestone had assumed its solid condition masses of molten matter were forced up from the interior of the Earth in some places crossing the beds and in others pushing between them now forming hard rock suitable for road metal. [People].
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392676 P804360] || [Bonsall]. Derbyshire, August 3rd 1914. [Group photo - large version of previous].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802601.jp2&y=305&x=529 Page 75]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392678 P804362] || Quarry in spheroidal dolerite - Pot Luck Farm (Drabble's Quarry), Bonsall. Derbyshire, August 3rd 1914. When the Carboniferous limestone had assumed its solid condition masses of molten matter were forced up from the interior of the Earth in some places crossing the beds and in others pushing between them now forming hard rock suitable for road metal. [People].
|-
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392677 P804361] || Quarry in Spheroidal Dolerite - Pot Luck Farm (Drabble's Quarry), Bonsall. Derbyshire, August 3rd 1914. When the Carboniferous limestone had assumed its solid condition masses of molten matter were forced up from the interior of the Earth in some places crossing the beds and in others pushing between them now forming hard rock suitable for road metal. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802601.jp2&y=305&x=529 Page 75]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392679 P804363] || ??????. Derbyshire, August 3rd 1914. In the process of cooling and contraction this rock frequently assumes a columnar structure and often divided by cross joints. In this case instead of being angular each segment owing to weathering takes a spheroidal form. It is stated that the cause of this is owing to the middle of each spheroid being a centre of crystallisation around which the different minerals of the rock arranged themselves.
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392678 P804362] || Quarry in spheroidal dolerite - Pot Luck Farm (Drabble's Quarry), Bonsall. Derbyshire, August 3rd 1914. When the Carboniferous limestone had assumed its solid condition masses of molten matter were forced up from the interior of the Earth in some places crossing the beds and in others pushing between them now forming hard rock suitable for road metal. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802601.jp2&y=305&x=529 Page 75]
|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392680 P804364] || ???????. Derbyshire, August 3rd 1914. In the process of cooling and contraction this rock frequently assumes a columnar structure and often divided by cross joints. In this case instead of being angular each segment owing to weathering takes a spheroidal form. It is stated that the cause of this is owing to the middle of each spheroid being a centre of crystallisation around which the different minerals of the rock arranged themselves.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392679 P804363] || ??????. Derbyshire, August 3rd 1914. In the process of cooling and contraction this rock frequently assumes a columnar structure and often divided by cross joints. In this case instead of being angular each segment owing to weathering takes a spheroidal form. It is stated that the cause of this is owing to the middle of each spheroid being a centre of crystallisation around which the different minerals of the rock arranged themselves.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802603.jp2&y=305&x=531 Page 77]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392681 P804365] || The valley of the Derwent from near Masson Hill looking along Darley Dale. Derbyshire, August 3rd 1914.  
|-
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392680 P804364] || ???????. Derbyshire, August 3rd 1914. In the process of cooling and contraction this rock frequently assumes a columnar structure and often divided by cross joints. In this case instead of being angular each segment owing to weathering takes a spheroidal form. It is stated that the cause of this is owing to the middle of each spheroid being a centre of crystallisation around which the different minerals of the rock arranged themselves.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802603.jp2&y=305&x=531 Page 77]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392682 P804366] || Limestone quarry, Matlock Bridge. This is in thinly bedded cherty limestones and contains fossils that show that it is of the subzone known as D3. Derbyshire, August 3rd 1914.  
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392681 P804365] || The valley of the Derwent from near Masson Hill looking along Darley Dale. Derbyshire, August 3rd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802603.jp2&y=305&x=531 Page 77]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392683 P804367] || The High Tor and Gorge of the Derwent through the Mountain Limestone which extends as far as Willersley when the river then winds through more open valleys to Derby and thence on to the Trent. Derbyshire, August 3rd 1914.  
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392682 P804366] || Limestone quarry, Matlock Bridge. This is in thinly bedded cherty limestones and contains fossils that show that it is of the subzone known as D3. Derbyshire, August 3rd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802605.jp2&y=305&x=533 Page 79]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392684 P804368] || Tufa Quarry, Matlock Bath. The circular holes were originally branches of trees coated by tufa. In course of time the wood decayed thus leaving spaces like pipes. Derbyshire, August 3rd 1914.  
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392683 P804367] || The High Tor and Gorge of the Derwent through the Mountain Limestone which extends as far as Willersley when the river then winds through more open valleys to Derby and thence on to the Trent. Derbyshire, August 3rd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802605.jp2&y=305&x=533 Page 79]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392685 P804369] || The more solid pieces are used for building purposes, but the porous portions are only fit for rock gardens. Derbyshire, August 3rd 1914.  
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392684 P804368] || Tufa Quarry, Matlock Bath. The circular holes were originally branches of trees coated by tufa. In course of time the wood decayed thus leaving spaces like pipes. Derbyshire, August 3rd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802605.jp2&y=305&x=533 Page 79]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392686 P804370] || Tufa. Matlock Bath. Derbyshire, August 3rd 1914. A mass of twigs coated with tufa from the above quarry.
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|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392685 P804369] || The more solid pieces are used for building purposes, but the porous portions are only fit for rock gardens. Derbyshire, August 3rd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802607.jp2&y=305&x=535 Page 81]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392687 P804371] || Tufa. Matlock Bath. Derbyshire, August 3rd 1914. Tufa which also goes by the name of travertin [travertine] or calcareous sinter is a deposit of carbonate of lime thrown down by springs which flow through beds of limestone. In this case at Matlock these specimens are from lime obtained from the Carboniferous limestone. The rain in passing through the atmosphere takes up Carbonic acid and assisted by humic acid from the soil when it sinks into the limestone dissolves portions of it away. When it comes to the surface again in the form of springs it loses some of the carbonic acid and the lime is thrown down in the form of tufa and incrusting any object that happens to be present.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392686 P804370] || Tufa. Matlock Bath. Derbyshire, August 3rd 1914. A mass of twigs coated with tufa from the above quarry.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802607.jp2&y=305&x=535 Page 81]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392688 P804372] || Tufa. Matlock Bath. Derbyshire, August 3rd 1914. Tufa which also goes by the name of travertin [travertine] or calcareous sinter is a deposit of carbonate of lime thrown down by springs which flow through beds of limestone. In this case at Matlock these specimens are from lime obtained from the Carboniferous limestone. The rain in passing through the atmosphere takes up Carbonic acid and assisted by humic acid from the soil when it sinks into the limestone dissolves portions of it away. When it comes to the surface again in the form of springs it loses some of the carbonic acid and the lime is thrown down in the form of tufa and incrusting any object that happens to be present.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392687 P804371] || Tufa. Matlock Bath. Derbyshire, August 3rd 1914. Tufa which also goes by the name of travertin [travertine] or calcareous sinter is a deposit of carbonate of lime thrown down by springs which flow through beds of limestone. In this case at Matlock these specimens are from lime obtained from the Carboniferous limestone. The rain in passing through the atmosphere takes up Carbonic acid and assisted by humic acid from the soil when it sinks into the limestone dissolves portions of it away. When it comes to the surface again in the form of springs it loses some of the carbonic acid and the lime is thrown down in the form of tufa and incrusting any object that happens to be present.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802607.jp2&y=305&x=535 Page 81]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392689 P804373] || Tufa. Matlock Bath. Derbyshire, August 3rd 1914. Tufa which also goes by the name of Travertin [Travertine] or Calcareous Sinter is a deposit of Carbonate of Lime thrown down by springs which flow through beds of limestone. In this case at Matlock these specimens are from lime obtained from the Carboniferous limestone. The rain in passing through the atmosphere takes up Carbonic acid and assisted by humic acid from the soil when it sinks into the limestone dissolves portions of it away. When it comes to the surface again in the form of springs it loses some of the carbonic acid and the lime is thrown down in the form of tufa and incrusting any object that happens to be present.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392688 P804372] || Tufa. Matlock Bath. Derbyshire, August 3rd 1914. Tufa which also goes by the name of travertin [travertine] or calcareous sinter is a deposit of carbonate of lime thrown down by springs which flow through beds of limestone. In this case at Matlock these specimens are from lime obtained from the Carboniferous limestone. The rain in passing through the atmosphere takes up Carbonic acid and assisted by humic acid from the soil when it sinks into the limestone dissolves portions of it away. When it comes to the surface again in the form of springs it loses some of the carbonic acid and the lime is thrown down in the form of tufa and incrusting any object that happens to be present.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802607.jp2&y=305&x=535 Page 81]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392690 P804374] || Tufa which also goes by the name of travertin [travertine] or calcareous sinter is a deposit of carbonate of lime thrown down by springs which flow through beds of limestone. Derbyshire, August 3rd 1914. In this case at Matlock these specimens are from lime obtained from the Carboniferous limestone. The rain in passing through the atmosphere takes up Carbonic acid and assisted by humic acid from the soil when it sinks into the limestone dissolves portions of it away. When it comes to the surface again in the form of springs it loses some of the carbonic acid and the lime is thrown down in the form of tufa and incrusting any object that happens to be present.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392689 P804373] || Tufa. Matlock Bath. Derbyshire, August 3rd 1914. Tufa which also goes by the name of Travertin [Travertine] or Calcareous Sinter is a deposit of Carbonate of Lime thrown down by springs which flow through beds of limestone. In this case at Matlock these specimens are from lime obtained from the Carboniferous limestone. The rain in passing through the atmosphere takes up Carbonic acid and assisted by humic acid from the soil when it sinks into the limestone dissolves portions of it away. When it comes to the surface again in the form of springs it loses some of the carbonic acid and the lime is thrown down in the form of tufa and incrusting any object that happens to be present.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802609.jp2&y=305&x=537 Page 83]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392691 P804375] || Carlton Hill Vent. Derbyshire, August 4th 1914. The volcanoes from which the Derbyshire Toadstone was thrown out have long been buried under later deposits on the sea bottom but in places where these deposits have been cleared away were are able to see the necks or pipes through which the molten lava was forced up. Carlton Hill is one of these necks filled with Agglomerate and Basalt containing olivine nodules. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392690 P804374] || Tufa which also goes by the name of travertin [travertine] or calcareous sinter is a deposit of carbonate of lime thrown down by springs which flow through beds of limestone. Derbyshire, August 3rd 1914. In this case at Matlock these specimens are from lime obtained from the Carboniferous limestone. The rain in passing through the atmosphere takes up Carbonic acid and assisted by humic acid from the soil when it sinks into the limestone dissolves portions of it away. When it comes to the surface again in the form of springs it loses some of the carbonic acid and the lime is thrown down in the form of tufa and incrusting any object that happens to be present.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802609.jp2&y=305&x=537 Page 83]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392692 P804376] || Carlton Hill Vent. Derbyshire, August 4th 1914. The volcanoes from which the Derbyshire Toadstone was thrown out have long been buried under later deposits on the sea bottom but in places where these deposits have been cleared away were are able to see the necks or pipes through which the molten lava was forced up. Carlton Hill is one of these necks filled with Agglomerate and Basalt containing olivine nodules. [Person].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392691 P804375] || Carlton Hill Vent. Derbyshire, August 4th 1914. The volcanoes from which the Derbyshire Toadstone was thrown out have long been buried under later deposits on the sea bottom but in places where these deposits have been cleared away were are able to see the necks or pipes through which the molten lava was forced up. Carlton Hill is one of these necks filled with Agglomerate and Basalt containing olivine nodules. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802609.jp2&y=305&x=537 Page 83]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392693 P804377] || Owing to the combined result of crystallization and cooling causing contraction the Basalt weathers into a mass of rough spheroides. Derbyshire, August 4th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392692 P804376] || Carlton Hill Vent. Derbyshire, August 4th 1914. The volcanoes from which the Derbyshire Toadstone was thrown out have long been buried under later deposits on the sea bottom but in places where these deposits have been cleared away were are able to see the necks or pipes through which the molten lava was forced up. Carlton Hill is one of these necks filled with Agglomerate and Basalt containing olivine nodules. [Person].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802609.jp2&y=305&x=537 Page 83]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392694 P804378] || The Gorge of the River Wye through Carboniferous Limestone. Derbyshire, August 4th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392693 P804377] || Owing to the combined result of crystallization and cooling causing contraction the Basalt weathers into a mass of rough spheroides. Derbyshire, August 4th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802611.jp2&y=305&x=539 Page 85]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392695 P804379] || Upper Lava resting on Carboniferous Limestone at Knott [Knot] Low, Millers Dale. Derbyshire, August 4th 1914. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392694 P804378] || The Gorge of the River Wye through Carboniferous Limestone. Derbyshire, August 4th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802611.jp2&y=305&x=539 Page 85]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392696 P804380] || Upper Lava resting on Carboniferous Limestone at Knott [Knot] Low, Millers Dale. Derbyshire, August 4th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392695 P804379] || Upper Lava resting on Carboniferous Limestone at Knott [Knot] Low, Millers Dale. Derbyshire, August 4th 1914. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802611.jp2&y=305&x=539 Page 85]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392697 P804381] || Ice-Scratched Boulder. Boulder Clay. Alport. Rowsley. Derbyshire, August 4th 1914.  
|}
== Excursion to Lyme Regis, May-June, 1914 ==
{| class="wikitable"
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392696 P804380] || Upper Lava resting on Carboniferous Limestone at Knott [Knot] Low, Millers Dale. Derbyshire, August 4th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802615.jp2&y=305&x=543 Page 89]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392698 P804382] || Lyme Regis looking West. Excursion to Lyme Regis, May 30th 1914. The town is built on the clayey portion of the Lias which is seen in the upper part of its cliffs. The limestones or Blue Lias are not seen in the town being bent downwards in the trough of a synclinal curve which bends the beds down to sea level.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392697 P804381] || Ice-Scratched Boulder. Boulder Clay. Alport. Rowsley. Derbyshire, August 4th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802615.jp2&y=305&x=543 Page 89]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392699 P804383] || Lyme Regis looking West. Excursion to Lyme Regis, May 30th 1914. The town is built on the clayey portion of the Lias which is seen in the upper part of its cliffs. The limestones or Blue Lias are not seen in the town being bent downwards in the trough of a synclinal curve which bends the beds down to sea level.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392698 P804382] || Lyme Regis looking West. Excursion to Lyme Regis, May 30th 1914. The town is built on the clayey portion of the Lias which is seen in the upper part of its cliffs. The limestones or Blue Lias are not seen in the town being bent downwards in the trough of a synclinal curve which bends the beds down to sea level.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802615.jp2&y=305&x=543 Page 89]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392700 P804384] || Looking East from just west of the Cobb. The cliffs in the distance are , on the left Stonebarrow, the high one in the centre is Golden Cap with Thorncombe Beacon beyond. Excursion to Lyme Regis, May 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392699 P804383] || Lyme Regis looking West. Excursion to Lyme Regis, May 30th 1914. The town is built on the clayey portion of the Lias which is seen in the upper part of its cliffs. The limestones or Blue Lias are not seen in the town being bent downwards in the trough of a synclinal curve which bends the beds down to sea level.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802615.jp2&y=305&x=543 Page 89]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392701 P804385] || The Harbour of Lyme known as the Cobb. This is built of Cowstones within and faced with Portland Roach. Excursion to Lyme Regis, May 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392700 P804384] || Looking East from just west of the Cobb. The cliffs in the distance are , on the left Stonebarrow, the high one in the centre is Golden Cap with Thorncombe Beacon beyond. Excursion to Lyme Regis, May 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802617.jp2&y=305&x=545 Page 91]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392702 P804386] || Church Cliffs - Lyme Regis. Excursion to Lyme Regis, May 30th 1914. Looking N.E. from point about 290 yards N.E. of Lyme Church. Added note: Table Ledge, Glass Bottle, Top Q. [Quick], Verity, Best, 2nd and Rattle, Mid Quick.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392701 P804385] || The Harbour of Lyme known as the Cobb. This is built of Cowstones within and faced with Portland Roach. Excursion to Lyme Regis, May 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802617.jp2&y=305&x=545 Page 91]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392703 P804387] || Church Cliffs - Lyme Regis. Excursion to Lyme Regis, May 30th 1914. Looking N.W. from a point about 420 yards N.E. of Lyme Church. Added note: Grey, Glass Bottle, Top Quick, Verity, Best, Second, Rattle, Mid Quick, Gumption, 3rd Quick, Top Tape, 2nd Tape, Top Copper, Mongrel, 2nd Mongrel, Specketty.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392702 P804386] || Church Cliffs - Lyme Regis. Excursion to Lyme Regis, May 30th 1914. Looking N.E. from point about 290 yards N.E. of Lyme Church. Added note: Table Ledge, Glass Bottle, Top Q. [Quick], Verity, Best, 2nd and Rattle, Mid Quick.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802617.jp2&y=305&x=545 Page 91]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392704 P804388] || Church Cliffs - Lyme Regis. Excursion to Lyme Regis, May 30th 1914. Church Cliffs at about 360 yards N.E. of Lyme Church. Added note: Fish, Grey, Glass Bottle, Top Quick, Verity, Best, Second, Ratt [Rattle], M. Quick, Gumption, 3rd Quick, Top Tape, 2nd Tape, Top Copper, Mongrel.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392703 P804387] || Church Cliffs - Lyme Regis. Excursion to Lyme Regis, May 30th 1914. Looking N.W. from a point about 420 yards N.E. of Lyme Church. Added note: Grey, Glass Bottle, Top Quick, Verity, Best, Second, Rattle, Mid Quick, Gumption, 3rd Quick, Top Tape, 2nd Tape, Top Copper, Mongrel, 2nd Mongrel, Specketty.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802617.jp2&y=305&x=545 Page 91]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392705 P804389] || Church Cliffs - Lyme Regis. Excursion to Lyme Regis, May 30th 1914. Church Cliffs at about 220 yards N.E. of Lyme Church. Added note: Top Quick, Verity, Best, Second, Rattle, Mid Quick, Gumption.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392704 P804388] || Church Cliffs - Lyme Regis. Excursion to Lyme Regis, May 30th 1914. Church Cliffs at about 360 yards N.E. of Lyme Church. Added note: Fish, Grey, Glass Bottle, Top Quick, Verity, Best, Second, Ratt [Rattle], M. Quick, Gumption, 3rd Quick, Top Tape, 2nd Tape, Top Copper, Mongrel.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802619.jp2&y=305&x=547 Page 93]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392706 P804390] || Fault at Church Cliffs at about 260 yards N.E. of Lyme Church. Excursion to Lyme Regis, May 30th 1914. Added note: Grey Ledge, Glass Bottle, Top Quick, Verity, Best Bed, Second Bed, Rattle, Middle Quick, Gumption.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392705 P804389] || Church Cliffs - Lyme Regis. Excursion to Lyme Regis, May 30th 1914. Church Cliffs at about 220 yards N.E. of Lyme Church. Added note: Top Quick, Verity, Best, Second, Rattle, Mid Quick, Gumption.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802619.jp2&y=305&x=547 Page 93]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392707 P804391] || A view of Church Cliffs from very close to Lyme about 120 yards East of Lyme Church. Excursion to Lyme Regis, May 30th 1914. Added note: Grey Ledge, Glass Bottle, Top Quick, Verity, Best, 2nd Bed, Rattle.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392706 P804390] || Fault at Church Cliffs at about 260 yards N.E. of Lyme Church. Excursion to Lyme Regis, May 30th 1914. Added note: Grey Ledge, Glass Bottle, Top Quick, Verity, Best Bed, Second Bed, Rattle, Middle Quick, Gumption.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802619.jp2&y=305&x=547 Page 93]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392708 P804392] || Fault in centre of photograph. The downthrow is on the west or left hand side. Excursion to Lyme Regis, May 30th 1914. Added note: Glass Bottle, Top Quick, Verity, Best, 2nd, Rattle, Mid Quick, Gumption, Third Quick.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392707 P804391] || A view of Church Cliffs from very close to Lyme about 120 yards East of Lyme Church. Excursion to Lyme Regis, May 30th 1914. Added note: Grey Ledge, Glass Bottle, Top Quick, Verity, Best, 2nd Bed, Rattle.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802619.jp2&y=305&x=547 Page 93]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392709 P804393] || 5/8 of a mile N.W. of Lyme Church. This is on the western limb of the Church Cliffs Anticline and represents a local disturbance with slight faulting of the bedding. Excursion to Lyme Regis, May 30th 1914. Added note: Glass Bottle, Best, 2nd, Rattle, Mid Quick, Gumption, Third Quick. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392708 P804392] || Fault in centre of photograph. The downthrow is on the west or left hand side. Excursion to Lyme Regis, May 30th 1914. Added note: Glass Bottle, Top Quick, Verity, Best, 2nd, Rattle, Mid Quick, Gumption, Third Quick.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802621.jp2&y=305&x=549 Page 95]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392710 P804394] || The Burning Mound. This is composed of shales, iron pyrites and cement stones. Excursion to Lyme Regis, May 30th 1914. This so called 'volcano' took fire in 1908. Rapid decomposition of the iron pyrites induced by a particularly wet season acting on clay with much inflammable (butuminous) matter in its composition is supposed to account for the phenomenon. Added note: About 1/2 mile N.E. of Lyme Church.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392709 P804393] || 5/8 of a mile N.W. of Lyme Church. This is on the western limb of the Church Cliffs Anticline and represents a local disturbance with slight faulting of the bedding. Excursion to Lyme Regis, May 30th 1914. Added note: Glass Bottle, Best, 2nd, Rattle, Mid Quick, Gumption, Third Quick. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802621.jp2&y=305&x=549 Page 95]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392711 P804395] || The Burning Mound. This is composed of Shales, iron pyrites and cement stones. Excursion to Lyme Regis, May 30th 1914. This so called 'volcano' took fire in 1908. Rapid decomposition of the Iron Pyrites induced by a particularly wet season acting on clay with much inflammable (butuminous) matter in its composition is supposed to account for the phenomenon. Added note: About 1/2 mile N.E. of Lyme Church.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392710 P804394] || The Burning Mound. This is composed of shales, iron pyrites and cement stones. Excursion to Lyme Regis, May 30th 1914. This so called 'volcano' took fire in 1908. Rapid decomposition of the iron pyrites induced by a particularly wet season acting on clay with much inflammable (butuminous) matter in its composition is supposed to account for the phenomenon. Added note: About 1/2 mile N.E. of Lyme Church.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802621.jp2&y=305&x=549 Page 95]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392712 P804396] || Pieces of baked shale showing discolouration in concentric rings according to different degrees of burning. Excursion to Lyme Regis, May 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392711 P804395] || The Burning Mound. This is composed of Shales, iron pyrites and cement stones. Excursion to Lyme Regis, May 30th 1914. This so called 'volcano' took fire in 1908. Rapid decomposition of the Iron Pyrites induced by a particularly wet season acting on clay with much inflammable (butuminous) matter in its composition is supposed to account for the phenomenon. Added note: About 1/2 mile N.E. of Lyme Church.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802621.jp2&y=305&x=549 Page 95]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392713 P804397] || Pieces of baked shale showing discolouration in concentric rings according to different degrees of burning. Excursion to Lyme Regis, May 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392712 P804396] || Pieces of baked shale showing discolouration in concentric rings according to different degrees of burning. Excursion to Lyme Regis, May 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802623.jp2&y=305&x=551 Page 97]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392714 P804398] || General view of the Cliffs and Coast looking East from about 3/4 mile N.E. of Lyme Church. Excursion to Lyme Regis, May 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392713 P804397] || Pieces of baked shale showing discolouration in concentric rings according to different degrees of burning. Excursion to Lyme Regis, May 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802623.jp2&y=305&x=551 Page 97]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392715 P804399] || General view of the cliffs and coast looking East from about 3/4 mile N.E. Of Lyme Church. Excursion to Lyme Regis, May 30th 1914. Added note: Bel. [Belemnite] Marls, Stellaris Beds.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392714 P804398] || General view of the Cliffs and Coast looking East from about 3/4 mile N.E. of Lyme Church. Excursion to Lyme Regis, May 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802623.jp2&y=305&x=551 Page 97]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392716 P804400] || The face of Black Ven at about 800 yards West of the end of Lower Sea Lane. Charmouth Beach and just east of Black Ven Rocks. Excursion to Lyme Regis, May 30th 1914. Added note: Stellaris Beds, Birchi Bed.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392715 P804399] || General view of the cliffs and coast looking East from about 3/4 mile N.E. Of Lyme Church. Excursion to Lyme Regis, May 30th 1914. Added note: Bel. [Belemnite] Marls, Stellaris Beds.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802623.jp2&y=305&x=551 Page 97]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392717 P804401] || The face of Black Ven at about 800 yards West of the end of Lower Sea Lane. Charmouth Beach and just east of Black Ven Rocks. Excursion to Lyme Regis, May 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392716 P804400] || The face of Black Ven at about 800 yards West of the end of Lower Sea Lane. Charmouth Beach and just east of Black Ven Rocks. Excursion to Lyme Regis, May 30th 1914. Added note: Stellaris Beds, Birchi Bed.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802625.jp2&y=305&x=553 Page 99]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392718 P804402] || Black Ven looking in a N.E. direction from between Canary Ledges and Cockpits about 5/8 of a mile west of Charmouth Beach. Excursion to Lyme Regis, May 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392717 P804401] || The face of Black Ven at about 800 yards West of the end of Lower Sea Lane. Charmouth Beach and just east of Black Ven Rocks. Excursion to Lyme Regis, May 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802625.jp2&y=305&x=553 Page 99]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392719 P804403] || Black Ven looking in a N.E. direction from between Canary Ledges and Cockpits about 5/8 of a mile west of Charmouth Beach. Excursion to Lyme Regis, May 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392718 P804402] || Black Ven looking in a N.E. direction from between Canary Ledges and Cockpits about 5/8 of a mile west of Charmouth Beach. Excursion to Lyme Regis, May 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802625.jp2&y=305&x=553 Page 99]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392720 P804404] || Black Ven from the beach at Cockpits. Excursion to Lyme Regis, May 30th 1914. [Person].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392719 P804403] || Black Ven looking in a N.E. direction from between Canary Ledges and Cockpits about 5/8 of a mile west of Charmouth Beach. Excursion to Lyme Regis, May 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802627.jp2&y=305&x=555 Page 101]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392721 P804405] || Fault in the 'Shales-with-Beef' below the Birchi Bed. 'Beef' is a fibrous calcium carbonate. Excursion to Lyme Regis, May 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392720 P804404] || Black Ven from the beach at Cockpits. Excursion to Lyme Regis, May 30th 1914. [Person].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802627.jp2&y=305&x=555 Page 101]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392722 P804406] || An undulation accompanying a fault in the Shales-with-Beef. The strings of Beef vary in thickness from a fraction of an inch up to 2 or 3 inches. Even when extremely thin they are nearly always double. Excursion to Lyme Regis, May 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392721 P804405] || Fault in the 'Shales-with-Beef' below the Birchi Bed. 'Beef' is a fibrous calcium carbonate. Excursion to Lyme Regis, May 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802627.jp2&y=305&x=555 Page 101]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392723 P804407] || Limestone nodule in Shales with Beef. These nodules often occur in connection with the Beef strings. When this occurs the two halves of the beef string diverge and the nodule lies between the enwrapping layers. Excursion to Lyme Regis, May 30th 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392722 P804406] || An undulation accompanying a fault in the Shales-with-Beef. The strings of Beef vary in thickness from a fraction of an inch up to 2 or 3 inches. Even when extremely thin they are nearly always double. Excursion to Lyme Regis, May 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802629.jp2&y=305&x=557 Page 103]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392724 P804408] || White Lias (Rhaetic beds) and Blue Lias Limestones and Shales at Pinhay Bay. Excursion to Lyme Regis, May 31st 1914. The lower beds of the Rhaetic, the Black Avicular contorta shales can be seen at low tide on the foreshore but the Cotham Marble is not exposed owing no doubt to its coverings of beach shingle and boulders. It has however been observed at Charton Bay.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392723 P804407] || Limestone nodule in Shales with Beef. These nodules often occur in connection with the Beef strings. When this occurs the two halves of the beef string diverge and the nodule lies between the enwrapping layers. Excursion to Lyme Regis, May 30th 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802629.jp2&y=305&x=557 Page 103]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392725 P804409] || White Lias (Rhaetic beds) and Blue Lias Limestones and Shales at Pinhay Bay. Excursion to Lyme Regis, May 31st 1914. The lower beds of the Rhaetic, the Black Avicular contorta shales can be seen at low tide on the foreshore but the Cotham Marble is not exposed owing no doubt to its coverings of beach shingle and boulders. It has however been observed at Charton Bay.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392724 P804408] || White Lias (Rhaetic beds) and Blue Lias Limestones and Shales at Pinhay Bay. Excursion to Lyme Regis, May 31st 1914. The lower beds of the Rhaetic, the Black Avicular contorta shales can be seen at low tide on the foreshore but the Cotham Marble is not exposed owing no doubt to its coverings of beach shingle and boulders. It has however been observed at Charton Bay.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802629.jp2&y=305&x=557 Page 103]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392726 P804410] || The Rhaetic Beds . Excursion to Lyme Regis, May 31st 1914. The Rhaetic Beds mark the commencement of the physical changes which terminated the continental conditions of the Trias and ushered in the marine conditions of the Jurassic, changes that evidently were not brought about uniformly over the British area. Added note: White Lias.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392725 P804409] || White Lias (Rhaetic beds) and Blue Lias Limestones and Shales at Pinhay Bay. Excursion to Lyme Regis, May 31st 1914. The lower beds of the Rhaetic, the Black Avicular contorta shales can be seen at low tide on the foreshore but the Cotham Marble is not exposed owing no doubt to its coverings of beach shingle and boulders. It has however been observed at Charton Bay.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802629.jp2&y=305&x=557 Page 103]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392727 P804411] || The Rhaetic Beds . Excursion to Lyme Regis, May 31st 1914. The Rhaetic Beds mark the commencement of the physical changes which terminated the continental conditions of the Trias and ushered in the marine conditions of the Jurassic, changes that evidently were not brought about uniformly over the British area. Added note: Lias, White Lias or Rhaetic, Black shales.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392726 P804410] || The Rhaetic Beds . Excursion to Lyme Regis, May 31st 1914. The Rhaetic Beds mark the commencement of the physical changes which terminated the continental conditions of the Trias and ushered in the marine conditions of the Jurassic, changes that evidently were not brought about uniformly over the British area. Added note: White Lias.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802631.jp2&y=305&x=559 Page 105]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392728 P804412] || The White Lias is a white or cream coloured limestone hard and smooth grained in the lowest beds. Excursion to Lyme Regis, May 31st 1914. Some of the more marly beds contain pebble like concretions composed of limestone similar to the white limestone. These stand out on the weathered surface of the rock in small lumps and impart to it a comglomerate appearance.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392727 P804411] || The Rhaetic Beds . Excursion to Lyme Regis, May 31st 1914. The Rhaetic Beds mark the commencement of the physical changes which terminated the continental conditions of the Trias and ushered in the marine conditions of the Jurassic, changes that evidently were not brought about uniformly over the British area. Added note: Lias, White Lias or Rhaetic, Black shales.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802631.jp2&y=305&x=559 Page 105]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392729 P804413] || The White Lias is a white or cream coloured limestone hard and smooth grained in the lowest beds. Excursion to Lyme Regis, May 31st 1914. Some of the more marly beds contain pebble like concretions composed of limestone similar to the white limestone. These stand out on the weathered surface of the rock in small lumps and impart to it a comglomerate appearance. Added note: White Lias. [Person].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392728 P804412] || The White Lias is a white or cream coloured limestone hard and smooth grained in the lowest beds. Excursion to Lyme Regis, May 31st 1914. Some of the more marly beds contain pebble like concretions composed of limestone similar to the white limestone. These stand out on the weathered surface of the rock in small lumps and impart to it a comglomerate appearance.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802631.jp2&y=305&x=559 Page 105]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392730 P804414] || The White Lias is a white or cream coloured limestone hard and smooth grained in the lowest beds. Excursion to Lyme Regis, May 31st 1914. Some of the more marly beds contain pebble like concretions composed of limestone similar to the white limestone. These stand out on the weathered surface of the rock in small lumps and impart to it a comglomerate appearance. [Caption used as for above].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392729 P804413] || The White Lias is a white or cream coloured limestone hard and smooth grained in the lowest beds. Excursion to Lyme Regis, May 31st 1914. Some of the more marly beds contain pebble like concretions composed of limestone similar to the white limestone. These stand out on the weathered surface of the rock in small lumps and impart to it a comglomerate appearance. Added note: White Lias. [Person].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802631.jp2&y=305&x=559 Page 105]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392731 P804415] || The White Lias is a white or cream coloured limestone hard and smooth grained in the lowest beds. Excursion to Lyme Regis, May 31st 1914. Some of the more marly beds contain pebble like concretions composed of limestone similar to the white limestone. These stand out on the weathered surface of the rock in small lumps and impart to it a comglomerate appearance. [Caption used as for above].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392730 P804414] || The White Lias is a white or cream coloured limestone hard and smooth grained in the lowest beds. Excursion to Lyme Regis, May 31st 1914. Some of the more marly beds contain pebble like concretions composed of limestone similar to the white limestone. These stand out on the weathered surface of the rock in small lumps and impart to it a comglomerate appearance. [Caption used as for above].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802633.jp2&y=305&x=561 Page 107]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392732 P804416] || Fault in White Lias, Pinhay Bay. Excursion to Lyme Regis, May 31st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392731 P804415] || The White Lias is a white or cream coloured limestone hard and smooth grained in the lowest beds. Excursion to Lyme Regis, May 31st 1914. Some of the more marly beds contain pebble like concretions composed of limestone similar to the white limestone. These stand out on the weathered surface of the rock in small lumps and impart to it a comglomerate appearance. [Caption used as for above].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802633.jp2&y=305&x=561 Page 107]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392733 P804417] || Sea cave worn out by the sea in a disturbed portion of the White Lias. Excursion to Lyme Regis, May 31st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392732 P804416] || Fault in White Lias, Pinhay Bay. Excursion to Lyme Regis, May 31st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802633.jp2&y=305&x=561 Page 107]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392734 P804418] || [Coastal erosion]. Excursion to Lyme Regis, May 31st 1914. Owing to the combined action of frost and springs on the one hand and the waves on the other a great amount of waste is going on on this coast the sea lifting blocks out along planes of jointing when the waves dash them about and grind them up.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392733 P804417] || Sea cave worn out by the sea in a disturbed portion of the White Lias. Excursion to Lyme Regis, May 31st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802633.jp2&y=305&x=561 Page 107]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392735 P804419] || [Coastal erosion]. Excursion to Lyme Regis, May 31st 1914. Owing to the combined action of frost and springs on the one hand and the waves on the other a great amount of waste is going on on this coast the sea lifting blocks out along planes of jointing when the waves dash them about and grind them up.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392734 P804418] || [Coastal erosion]. Excursion to Lyme Regis, May 31st 1914. Owing to the combined action of frost and springs on the one hand and the waves on the other a great amount of waste is going on on this coast the sea lifting blocks out along planes of jointing when the waves dash them about and grind them up.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802635.jp2&y=305&x=563 Page 109]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392736 P804420] || Pinhay Bay. Excursion to Lyme Regis, May 31st 1914. Owing to the Easterly dip of the Lias beds it is quite easy to trace the upwards succession of these beds. At Pinhay Bay we start eastward along the shore when we see higher and higher beds of the Blue Lias series as we pass over them in succession. [photo is likely missing on this page].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392735 P804419] || [Coastal erosion]. Excursion to Lyme Regis, May 31st 1914. Owing to the combined action of frost and springs on the one hand and the waves on the other a great amount of waste is going on on this coast the sea lifting blocks out along planes of jointing when the waves dash them about and grind them up.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802635.jp2&y=305&x=563 Page 109]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392737 P804421] || [Limestone ledges]. Excursion to Lyme Regis, May 31st 1914. The beds of limestone or ledges cropping out on the sea shore. These form natural breakwaters but unfortunately the Lyme people allow a cement company to break them up and use them for export thus endangering the cliffs that protect the town.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392736 P804420] || Pinhay Bay. Excursion to Lyme Regis, May 31st 1914. Owing to the Easterly dip of the Lias beds it is quite easy to trace the upwards succession of these beds. At Pinhay Bay we start eastward along the shore when we see higher and higher beds of the Blue Lias series as we pass over them in succession. [photo is likely missing on this page].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802635.jp2&y=305&x=563 Page 109]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392738 P804422] || [Limestone ledges]. Excursion to Lyme Regis, May 31st 1914. The beds of limestone or ledges cropping out on the sea shore. These form natural breakwaters but unfortunately the Lyme people allow a cement company to break them up and use them for export thus endangering the cliffs that protect the town.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392737 P804421] || [Limestone ledges]. Excursion to Lyme Regis, May 31st 1914. The beds of limestone or ledges cropping out on the sea shore. These form natural breakwaters but unfortunately the Lyme people allow a cement company to break them up and use them for export thus endangering the cliffs that protect the town.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802637.jp2&y=305&x=565 Page 111]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392739 P804423] || ''Amaltheus Margaritatus''. Lyme Regis. Excursion to Lyme Regis, May 31st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392738 P804422] || [Limestone ledges]. Excursion to Lyme Regis, May 31st 1914. The beds of limestone or ledges cropping out on the sea shore. These form natural breakwaters but unfortunately the Lyme people allow a cement company to break them up and use them for export thus endangering the cliffs that protect the town.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802637.jp2&y=305&x=565 Page 111]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392740 P804424] || ''Asteroceras Brookei''. Lyme Regis. Excursion to Lyme Regis, May 31st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392739 P804423] || Amaltheus Margaritatus. Lyme Regis. Excursion to Lyme Regis, May 31st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802637.jp2&y=305&x=565 Page 111]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392741 P804425] || Large ammonites on surface of ledge near Seven Rock Point. This ammonite cemetery contains specimens from 12 to 18 inches in diameter. Excursion to Lyme Regis, May 31st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392740 P804424] || Asteroceras Brookei. Lyme Regis. Excursion to Lyme Regis, May 31st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802637.jp2&y=305&x=565 Page 111]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392742 P804426] || Large ammonites on surface of ledge near Seven Rock Point. This Ammonite Cemetery contains specimens from 12 to 18 inches in diameter. Excursion to Lyme Regis, May 31st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392741 P804425] || Large ammonites on surface of ledge near Seven Rock Point. This ammonite cemetery contains specimens from 12 to 18 inches in diameter. Excursion to Lyme Regis, May 31st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802639.jp2&y=305&x=567 Page 113]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392743 P804427] || Looking West over Charmouth from a field near the top of Stonebarrow Lane E. of Charmouth. Excursion to Lyme Regis, June 1st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392742 P804426] || Large ammonites on surface of ledge near Seven Rock Point. This Ammonite Cemetery contains specimens from 12 to 18 inches in diameter. Excursion to Lyme Regis, May 31st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802639.jp2&y=305&x=567 Page 113]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392744 P804428] || Looking E.N.E. from near the Lyme Road just East of the Bellows over Charmouth Village. Excursion to Lyme Regis, June 1st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392743 P804427] || Looking West over Charmouth from a field near the top of Stonebarrow Lane E. of Charmouth. Excursion to Lyme Regis, June 1st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802641.jp2&y=305&x=569 Page 115]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392745 P804429] || View of Charmouth Beach from Cockpits. The rocks in the foreground are the Canary Ledges, the first stages in a recent plane of marine denudation. Excursion to Lyme Regis, June 1st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392744 P804428] || Looking E.N.E. from near the Lyme Road just East of the Bellows over Charmouth Village. Excursion to Lyme Regis, June 1st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802641.jp2&y=305&x=569 Page 115]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392746 P804430] || Undulating strata at about the level of the Lower and Upper Cement Beds capped with much drift and Hill creep. Mouth of the River Char. Excursion to Lyme Regis, June 1st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392745 P804429] || View of Charmouth Beach from Cockpits. The rocks in the foreground are the Canary Ledges, the first stages in a recent plane of marine denudation. Excursion to Lyme Regis, June 1st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802643.jp2&y=305&x=571 Page 117]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392747 P804431] || The large amphitheatre shaped hollow in Stonebarrow Cliff immediately west of Fairy Dell. Excursion to Lyme Regis, June 1st 1914. Between June 1908 and 1909 a large fall occurred here exposing a fine section of the fault on the right or eastern side of the hollow. Added note: Drift, Foxmould, Sand of the Cowstone horizon, Gault.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392746 P804430] || Undulating strata at about the level of the Lower and Upper Cement Beds capped with much drift and Hill creep. Mouth of the River Char. Excursion to Lyme Regis, June 1st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802643.jp2&y=305&x=571 Page 117]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392748 P804432] || The large amphitheatre shaped hollow in Stonebarrow Cliff immediately west of Fairy Dell. Excursion to Lyme Regis, June 1st 1914. Between June 1908 and 1909 a large fall occurred here exposing a fine section of the fault on the right or eastern side of the hollow.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392747 P804431] || The large amphitheatre shaped hollow in Stonebarrow Cliff immediately west of Fairy Dell. Excursion to Lyme Regis, June 1st 1914. Between June 1908 and 1909 a large fall occurred here exposing a fine section of the fault on the right or eastern side of the hollow. Added note: Drift, Foxmould, Sand of the Cowstone horizon, Gault.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802643.jp2&y=305&x=571 Page 117]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392749 P804433] || The Western bank of the amphitheatre shaped hollow. Excursion to Lyme Regis, June 1st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392748 P804432] || The large amphitheatre shaped hollow in Stonebarrow Cliff immediately west of Fairy Dell. Excursion to Lyme Regis, June 1st 1914. Between June 1908 and 1909 a large fall occurred here exposing a fine section of the fault on the right or eastern side of the hollow.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802643.jp2&y=305&x=571 Page 117]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392750 P804434] || The Seaward Cliff below Fairy Dell in Belemnite Marls. Excursion to Lyme Regis, June 1st 1914. Added note: Belemnite Marls.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392749 P804433] || The Western bank of the amphitheatre shaped hollow. Excursion to Lyme Regis, June 1st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802645.jp2&y=305&x=573 Page 119]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392751 P804435] || Black Ven looking East from the Western end about 3/4 mile from both Charmouth and Lyme. Excursion to Lyme Regis, June 1st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392750 P804434] || The Seaward Cliff below Fairy Dell in Belemnite Marls. Excursion to Lyme Regis, June 1st 1914. Added note: Belemnite Marls.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802645.jp2&y=305&x=573 Page 119]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392752 P804436] || Black Ven looking East from the Western end about 3/4 mile from both Charmouth and Lyme. Excursion to Lyme Regis, June 1st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392751 P804435] || Black Ven looking East from the Western end about 3/4 mile from both Charmouth and Lyme. Excursion to Lyme Regis, June 1st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802645.jp2&y=305&x=573 Page 119]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392753 P804437] || Fairy Dell looking East from its extreme western end. Excursion to Lyme Regis, June 1st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392752 P804436] || Black Ven looking East from the Western end about 3/4 mile from both Charmouth and Lyme. Excursion to Lyme Regis, June 1st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802645.jp2&y=305&x=573 Page 119]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392754 P804438] || Fairy Dell looking East from its extreme western end. Excursion to Lyme Regis, June 1st 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392753 P804437] || Fairy Dell looking East from its extreme western end. Excursion to Lyme Regis, June 1st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802647.jp2&y=305&x=575 Page 121]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392755 P804439] || Ground Plan and Sections of the Great Landslip at Great and Little Bindon and Dowlands in the Parish of Axmouth on the East Coast of Devon, which took place on the 25th December 1839. Excursion to Lyme Regis, June 1st 1914. [Numbering on photos ignored]. [Many annotations on section not transcribed].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392754 P804438] || Fairy Dell looking East from its extreme western end. Excursion to Lyme Regis, June 1st 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802647.jp2&y=305&x=575 Page 121]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392756 P804440] || Geological Section of the Chasm, Undercliff and New Raised Beach. From the Eastern Boundary of Great Bindon to the Sea. Excursion to Lyme Regis, June 1st 1914. [Numbering on photos ignored]. [Many annotations on section not transcribed].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392755 P804439] || Ground Plan and Sections of the Great Landslip at Great and Little Bindon and Dowlands in the Parish of Axmouth on the East Coast of Devon, which took place on the 25th December 1839. Excursion to Lyme Regis, June 1st 1914. [Numbering on photos ignored]. [Many annotations on section not transcribed].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802647.jp2&y=305&x=575 Page 121]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392757 P804441] || Geological View of the Coast from Lyme Regis in the County of Devon to Axmouth Harbour on the East Coast of Devon. Excursion to Lyme Regis, June 1st 1914. [Left hand end of 4] [Numbering on photos ignored]. [Many annotations on section not transcribed].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392756 P804440] || Geological Section of the Chasm, Undercliff and New Raised Beach. From the Eastern Boundary of Great Bindon to the Sea. Excursion to Lyme Regis, June 1st 1914. [Numbering on photos ignored]. [Many annotations on section not transcribed].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802647.jp2&y=305&x=575 Page 121]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392758 P804442] || Geological View of the Coast from Lyme Regis in the County of Devon to Axmouth Harbour on the East Coast of Devon. Excursion to Lyme Regis, June 1st 1914. [Right hand end of 3] [Numbering on photos ignored]. [Many annotations on section not transcribed].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392757 P804441] || Geological View of the Coast from Lyme Regis in the County of Devon to Axmouth Harbour on the East Coast of Devon. Excursion to Lyme Regis, June 1st 1914. [Left hand end of 4] [Numbering on photos ignored]. [Many annotations on section not transcribed].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802649.jp2&y=305&x=577 Page 123]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392759 P804443] || A view of the Landslip from Great Bindon. Excursion to Lyme Regis, June 1st 1914. [Right hand end of 3] [Numbering on photos ignored].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392758 P804442] || Geological View of the Coast from Lyme Regis in the County of Devon to Axmouth Harbour on the East Coast of Devon. Excursion to Lyme Regis, June 1st 1914. [Right hand end of 3] [Numbering on photos ignored]. [Many annotations on section not transcribed].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802649.jp2&y=305&x=577 Page 123]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392760 P804444] || View of the Great Chasm from its Western end at Bindon. Excursion to Lyme Regis, June 1st 1914. [Right hand end of 3] [Numbering on photos ignored].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392759 P804443] || A view of the Landslip from Great Bindon. Excursion to Lyme Regis, June 1st 1914. [Right hand end of 3] [Numbering on photos ignored].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802651.jp2&y=305&x=579 Page 125]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392761 P804445] || View of the Landslip at Whitlands, about one mile to the Eastward of the great Chasm at Dowlands which took place on the 3rd of February 1840. Excursion to Lyme Regis, June 1st 1914. Pentire Haven - Contorted Frasnian beds [incorrect title]. [Artist's impression].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392760 P804444] || View of the Great Chasm from its Western end at Bindon. Excursion to Lyme Regis, June 1st 1914. [Right hand end of 3] [Numbering on photos ignored].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802651.jp2&y=305&x=579 Page 125]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392762 P804446] || Landslip under Southdown between Beer Head and Branscombe, which took place in 1789-90 looking Westward to Sidmouth Torbay and the Start Point. Excursion to Lyme Regis, June 1st 1914. Pentire Haven - Sill in Frasnian beds [incorrect title]. [Artist's impression].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392761 P804445] || View of the Landslip at Whitlands, about one mile to the Eastward of the great Chasm at Dowlands which took place on the 3rd of February 1840. Excursion to Lyme Regis, June 1st 1914. Pentire Haven - Contorted Frasnian beds [incorrect title]. [Artist's impression].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802651.jp2&y=305&x=579 Page 125]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392763 P804447] || View from the New Beach, looking Westward to Beer Head. Excursion to Lyme Regis, June 1st 1914. [Artist's impression].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392762 P804446] || Landslip under Southdown between Beer Head and Branscombe, which took place in 1789-90 looking Westward to Sidmouth Torbay and the Start Point. Excursion to Lyme Regis, June 1st 1914. Pentire Haven - Sill in Frasnian beds [incorrect title]. [Artist's impression].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802651.jp2&y=305&x=579 Page 125]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392764 P804448] || View from the Western end of the beach near Culverhole Point, looking Eastward. Excursion to Lyme Regis, June 1st 1914. [Artist's impression].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392763 P804447] || View from the New Beach, looking Westward to Beer Head. Excursion to Lyme Regis, June 1st 1914. [Artist's impression].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802653.jp2&y=305&x=581 Page 127]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392765 P804449] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392764 P804448] || View from the Western end of the beach near Culverhole Point, looking Eastward. Excursion to Lyme Regis, June 1st 1914. [Artist's impression].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802653.jp2&y=305&x=581 Page 127]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392766 P804450] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392765 P804449] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802653.jp2&y=305&x=581 Page 127]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392767 P804451] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392766 P804450] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802653.jp2&y=305&x=581 Page 127]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392768 P804452] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392767 P804451] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802655.jp2&y=305&x=583 Page 129]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392769 P804453] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392768 P804452] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802655.jp2&y=305&x=583 Page 129]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392770 P804454] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392769 P804453] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802655.jp2&y=305&x=583 Page 129]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392771 P804455] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392770 P804454] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802655.jp2&y=305&x=583 Page 129]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392772 P804456] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392771 P804455] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802657.jp2&y=305&x=585 Page 131]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392773 P804457] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392772 P804456] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802657.jp2&y=305&x=585 Page 131]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392774 P804458] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392773 P804457] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802657.jp2&y=305&x=585 Page 131]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392775 P804459] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392774 P804458] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802657.jp2&y=305&x=585 Page 131]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392776 P804460] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392775 P804459] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802659.jp2&y=305&x=587 Page 133]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392777 P804461] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392776 P804460] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802659.jp2&y=305&x=587 Page 133]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392778 P804462] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392777 P804461] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802659.jp2&y=305&x=587 Page 133]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392779 P804463] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392778 P804462] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802659.jp2&y=305&x=587 Page 133]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392780 P804464] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392779 P804463] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802661.jp2&y=305&x=589 Page 135]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392781 P804465] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392780 P804464] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802661.jp2&y=305&x=589 Page 135]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392782 P804466] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392781 P804465] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802661.jp2&y=305&x=589 Page 135]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392783 P804467] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392782 P804466] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802661.jp2&y=305&x=589 Page 135]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392784 P804468] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392783 P804467] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802663.jp2&y=305&x=591 Page 137]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392785 P804469] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392784 P804468] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802663.jp2&y=305&x=591 Page 137]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392786 P804470] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392785 P804469] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802663.jp2&y=305&x=591 Page 137]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392787 P804471] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392786 P804470] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802663.jp2&y=305&x=591 Page 137]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392788 P804472] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392787 P804471] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802665.jp2&y=305&x=593 Page 139]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392789 P804473] || The Great Cleft is a fissure running parallel to the face of the cliff thus cutting off a thick slide of rock. Excursion to Lyme Regis, June 2nd 1914. The crack first started in 1886 and had gradually widened year by year but rather more rapidly of late than at first. The base is cut in Upper Greensand the cherty nature of which is is [sic] well seen. Next comes the Lower Chalk about 3ft thick and then White Chalk of the zone of Rhynchonella cuvieri 60 feet thick followed by 71 feet of Terebratulina gracilis zone.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392788 P804472] || The Landslip. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802665.jp2&y=305&x=593 Page 139]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392790 P804474] || The Great Cleft is a fissure running parallel to the face of the cliff thus cutting off a thick slide of rock. Excursion to Lyme Regis, June 2nd 1914. The crack first started in 1886 and had gradually widened year by year but rather more rapidly of late than at first. The base is cut in Upper Greensand the cherty nature of which is is [sic] well seen. Next comes the Lower Chalk about 3ft thick and then White Chalk of the zone of Rhynchonella cuvieri 60 feet thick followed by 71 feet of Terebratulina gracilis zone.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392789 P804473] || The Great Cleft is a fissure running parallel to the face of the cliff thus cutting off a thick slide of rock. Excursion to Lyme Regis, June 2nd 1914. The crack first started in 1886 and had gradually widened year by year but rather more rapidly of late than at first. The base is cut in Upper Greensand the cherty nature of which is is [sic] well seen. Next comes the Lower Chalk about 3ft thick and then White Chalk of the zone of Rhynchonella cuvieri 60 feet thick followed by 71 feet of Terebratulina gracilis zone.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802665.jp2&y=305&x=593 Page 139]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392791 P804475] || The Great Cleft is a fissure running parallel to the face of the cliff thus cutting off a thick slide of rock. Excursion to Lyme Regis, June 2nd 1914. The crack first started in 1886 and had gradually widened year by year but rather more rapidly of late than at first. The base is cut in Upper Greensand the cherty nature of which is is [sic] well seen. Next comes the Lower Chalk about 3ft thick and then White Chalk of the zone of Rhynchonella cuvieri 60 feet thick followed by 71 feet of Terebratulina gracilis zone.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392790 P804474] || The Great Cleft is a fissure running parallel to the face of the cliff thus cutting off a thick slide of rock. Excursion to Lyme Regis, June 2nd 1914. The crack first started in 1886 and had gradually widened year by year but rather more rapidly of late than at first. The base is cut in Upper Greensand the cherty nature of which is is [sic] well seen. Next comes the Lower Chalk about 3ft thick and then White Chalk of the zone of Rhynchonella cuvieri 60 feet thick followed by 71 feet of Terebratulina gracilis zone.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802665.jp2&y=305&x=593 Page 139]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392792 P804476] || The Great Cleft is a fissure running parallel to the face of the cliff thus cutting off a thick slide of rock. Excursion to Lyme Regis, June 2nd 1914. The crack first started in 1886 and had gradually widened year by year but rather more rapidly of late than at first. The base is cut in Upper Greensand the cherty nature of which is is [sic] well seen. Next comes the Lower Chalk about 3ft thick and then White Chalk of the zone of Rhynchonella cuvieri 60 feet thick followed by 71 feet of Terebratulina gracilis zone.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392791 P804475] || The Great Cleft is a fissure running parallel to the face of the cliff thus cutting off a thick slide of rock. Excursion to Lyme Regis, June 2nd 1914. The crack first started in 1886 and had gradually widened year by year but rather more rapidly of late than at first. The base is cut in Upper Greensand the cherty nature of which is is [sic] well seen. Next comes the Lower Chalk about 3ft thick and then White Chalk of the zone of Rhynchonella cuvieri 60 feet thick followed by 71 feet of Terebratulina gracilis zone.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802667.jp2&y=305&x=595 Page 141]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392793 P804477] || The Chapel Rock. Excursion to Lyme Regis, June 2nd 1914. The Chapel Rock is a lofty detached mass of Chalk of the zones of Terebratulina gracilis, Holaster planus, and Micraster cor-testudinarium which has slipped from the main face of Pinhay Cliffs. It is between 120 and 130 ft high.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392792 P804476] || The Great Cleft is a fissure running parallel to the face of the cliff thus cutting off a thick slide of rock. Excursion to Lyme Regis, June 2nd 1914. The crack first started in 1886 and had gradually widened year by year but rather more rapidly of late than at first. The base is cut in Upper Greensand the cherty nature of which is is [sic] well seen. Next comes the Lower Chalk about 3ft thick and then White Chalk of the zone of Rhynchonella cuvieri 60 feet thick followed by 71 feet of Terebratulina gracilis zone.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802667.jp2&y=305&x=595 Page 141]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392794 P804478] || The Chapel Rock. Excursion to Lyme Regis, June 2nd 1914. The Chapel Rock is a lofty detached mass of Chalk of the zones of Terebratulina gracilis, Holaster planus, and Micraster cor-testudinarium which has slipped from the main face of Pinhay Cliffs. It is between 120 and 130 ft high.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392793 P804477] || The Chapel Rock. Excursion to Lyme Regis, June 2nd 1914. The Chapel Rock is a lofty detached mass of Chalk of the zones of Terebratulina gracilis, Holaster planus, and Micraster cor-testudinarium which has slipped from the main face of Pinhay Cliffs. It is between 120 and 130 ft high.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802667.jp2&y=305&x=595 Page 141]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392795 P804479] || ''Rhacoceras loscombei''. Lyme Regis. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392794 P804478] || The Chapel Rock. Excursion to Lyme Regis, June 2nd 1914. The Chapel Rock is a lofty detached mass of Chalk of the zones of Terebratulina gracilis, Holaster planus, and Micraster cor-testudinarium which has slipped from the main face of Pinhay Cliffs. It is between 120 and 130 ft high.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802667.jp2&y=305&x=595 Page 141]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392796 P804480] || ''Rhacoceras loscombei''. Lyme Regis. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392795 P804479] || Rhacoceras Loscombei. Lyme Regis. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802669.jp2&y=305&x=597 Page 143]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392797 P804481] || Charton Bay. Excursion to Lyme Regis, June 2nd 1914. The higher portions are seen to include the Black Shales and White Lias estimated to be 25 feet thick while the lower portions consist of alternations of hard and soft marls passing gradually into the red and green marls of the Keuper.
|-
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392796 P804480] || Rhacoceras Loscombei. Lyme Regis. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802669.jp2&y=305&x=597 Page 143]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392798 P804482] || Charton Bay. Excursion to Lyme Regis, June 2nd 1914. The higher portions are seen to include the Black Shales and White Lias estimated to be 25 feet thick while the lower portions consist of alternations of hard and soft marls passing gradually into the red and green marls of the Keuper.
|-
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| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392797 P804481] || Charton Bay. Excursion to Lyme Regis, June 2nd 1914. The higher portions are seen to include the Black Shales and White Lias estimated to be 25 feet thick while the lower portions consist of alternations of hard and soft marls passing gradually into the red and green marls of the Keuper.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802669.jp2&y=305&x=597 Page 143]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392799 P804483] || Pinhay Bay. This ravine and watercourse coincides with a fault that throws down the Blue Lias limestones some 40 feet on the west. On the east the lowest beds of the Lias are seen resting on the White Lias. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392798 P804482] || Charton Bay. Excursion to Lyme Regis, June 2nd 1914. The higher portions are seen to include the Black Shales and White Lias estimated to be 25 feet thick while the lower portions consist of alternations of hard and soft marls passing gradually into the red and green marls of the Keuper.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802669.jp2&y=305&x=597 Page 143]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392800 P804484] || Humble Point. Excursion to Lyme Regis, June 2nd 1914.  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392799 P804483] || Pinhay Bay. This ravine and watercourse coincides with a fault that throws down the Blue Lias limestones some 40 feet on the west. On the east the lowest beds of the Lias are seen resting on the White Lias. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802671.jp2&y=305&x=599 Page 145]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392801 P804485] || Excursion to Lyme Regis, June 2nd 1914. [Person].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392800 P804484] || Humble Point. Excursion to Lyme Regis, June 2nd 1914.  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802671.jp2&y=305&x=599 Page 145]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392802 P804486] || Excursion to Lyme Regis, June 2nd 1914. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392801 P804485] || Excursion to Lyme Regis, June 2nd 1914. [Person].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802671.jp2&y=305&x=599 Page 145]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392803 P804487] || At Charton Bay the entire sequence of the Rhaetic Beds can be seen. Excursion to Lyme Regis, June 2nd 1914. The beds are bent into a gentle anticline at the base of which traces of grey marls with reddish tinges may be detected. Above come the grey marls with shale beds, greenish marls and laminated mudstones. Then the Black Shales followed by mammillated Landscape stone and capped by White Lias. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392802 P804486] || Excursion to Lyme Regis, June 2nd 1914. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802671.jp2&y=305&x=599 Page 145]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392804 P804488] || At Charton Bay the entire sequence of the Rhaetic Beds can be seen. Excursion to Lyme Regis, June 2nd 1914. The beds are bent into a gentle anticline at the base of which traces of grey marls with reddish tinges may be detected. Above come the grey marls with shale beds, greenish marls and laminated mudstones. Then the Black Shales followed by mammillated Landscape stone and capped by White Lias. [People].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392803 P804487] || At Charton Bay the entire sequence of the Rhaetic Beds can be seen. Excursion to Lyme Regis, June 2nd 1914. The beds are bent into a gentle anticline at the base of which traces of grey marls with reddish tinges may be detected. Above come the grey marls with shale beds, greenish marls and laminated mudstones. Then the Black Shales followed by mammillated Landscape stone and capped by White Lias. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802673.jp2&y=305&x=601 Page 147]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392805 P804489] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. On the West side of the Valley of the Axe at South Down between Beer and Branscombe a very considerable landslip occurred in March 1790 which for importance and picturesque effect was unrivalled until the later convulsion at Bindon.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392804 P804488] || At Charton Bay the entire sequence of the Rhaetic Beds can be seen. Excursion to Lyme Regis, June 2nd 1914. The beds are bent into a gentle anticline at the base of which traces of grey marls with reddish tinges may be detected. Above come the grey marls with shale beds, greenish marls and laminated mudstones. Then the Black Shales followed by mammillated Landscape stone and capped by White Lias. [People].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802673.jp2&y=305&x=601 Page 147]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392806 P804490] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. Here in the middle of the night a tract of from seven to ten acres ranging along the brow of a steep cliff immediately overhanging the sea suddenly sank down from 200 to 260 feet presenting a striking group of shattered pinnacles and columns of chalk intermingled with the sunken fragments of the fields thus torn awar from their native site.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392805 P804489] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. On the West side of the Valley of the Axe at South Down between Beer and Branscombe a very considerable landslip occurred in March 1790 which for importance and picturesque effect was unrivalled until the later convulsion at Bindon.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802673.jp2&y=305&x=601 Page 147]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392807 P804491] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The remains of hedges still traversed these fragments and a stile was seen undisturbed on the summit of one of the subsided columnar masses. The eye looking from above on this wild scene of ruin saw it finely backed by the deep blue of the channel beneath for in this case the landslip in question formed the first term in the commencement of a new and incipient undercliff which fresh falls and the lapse of centuries will be required to bring into the state of that between Lyme and Seaton.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392806 P804490] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. Here in the middle of the night a tract of from seven to ten acres ranging along the brow of a steep cliff immediately overhanging the sea suddenly sank down from 200 to 260 feet presenting a striking group of shattered pinnacles and columns of chalk intermingled with the sunken fragments of the fields thus torn awar from their native site.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802673.jp2&y=305&x=601 Page 147]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392808 P804492] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The remains of hedges still traversed these fragments and a stile was seen undisturbed on the summit of one of the subsided columnar masses. The eye looking from above on this wild scene of ruin saw it finely backed by the deep blue of the channel beneath for in this case the landslip in question formed the first term in the commencement of a new and incipient undercliff which fresh falls and the lapse of centuries will be required to bring into the state of that between Lyme and Seaton.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392807 P804491] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The remains of hedges still traversed these fragments and a stile was seen undisturbed on the summit of one of the subsided columnar masses. The eye looking from above on this wild scene of ruin saw it finely backed by the deep blue of the channel beneath for in this case the landslip in question formed the first term in the commencement of a new and incipient undercliff which fresh falls and the lapse of centuries will be required to bring into the state of that between Lyme and Seaton.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802675.jp2&y=305&x=603 Page 149]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392809 P804493] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. It is stated that many previous symptoms had foreshown this catastrophe. A fissure had opened along the line where the disruption afterwards occurred, for months before the subsidence ensued. Another previous sign was given by the stoppage about two years before of a copious stream of very fine water which used to flow out and just below the freestone quarry opened then as now about the middle of the cliff.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392808 P804492] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The remains of hedges still traversed these fragments and a stile was seen undisturbed on the summit of one of the subsided columnar masses. The eye looking from above on this wild scene of ruin saw it finely backed by the deep blue of the channel beneath for in this case the landslip in question formed the first term in the commencement of a new and incipient undercliff which fresh falls and the lapse of centuries will be required to bring into the state of that between Lyme and Seaton.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802675.jp2&y=305&x=603 Page 149]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392810 P804494] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. It is stated that many previous symptoms had foreshown this catastrophe. A fissure had opened along the line where the disruption afterwards occurred, for months before the subsidence ensued. Another previous sign was given by the stoppage about two years before of a copious stream of very fine water which used to flow out and just below the freestone quarry opened then as now about the middle of the cliff.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392809 P804493] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. It is stated that many previous symptoms had foreshown this catastrophe. A fissure had opened along the line where the disruption afterwards occurred, for months before the subsidence ensued. Another previous sign was given by the stoppage about two years before of a copious stream of very fine water which used to flow out and just below the freestone quarry opened then as now about the middle of the cliff.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802675.jp2&y=305&x=603 Page 149]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392811 P804495] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The strong persuasion of the neighbours connects this with the cause of the subsequent convulsion and the probable opinion is that it had forced a new channel through some of the fissures which were then opening. A fresh stream broke out after the landslip nearer the beach.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392810 P804494] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. It is stated that many previous symptoms had foreshown this catastrophe. A fissure had opened along the line where the disruption afterwards occurred, for months before the subsidence ensued. Another previous sign was given by the stoppage about two years before of a copious stream of very fine water which used to flow out and just below the freestone quarry opened then as now about the middle of the cliff.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802675.jp2&y=305&x=603 Page 149]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392812 P804496] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The strong persuasion of the neighbours connects this with the cause of the subsequent convulsion and the probable opinion is that it had forced a new channel through some of the fissures which were then opening. A fresh stream broke out after the landslip nearer the beach.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392811 P804495] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The strong persuasion of the neighbours connects this with the cause of the subsequent convulsion and the probable opinion is that it had forced a new channel through some of the fissures which were then opening. A fresh stream broke out after the landslip nearer the beach.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802677.jp2&y=305&x=605 Page 151]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392813 P804497] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The subsided mass pressed forward into the sea so as to approach within 100 yards of a submarine crag called the Sherborne Rock which before then was about 400 yards from the coast line. This subsidence was attended by the same phenomenon as at Culverhole and Whitelands namely the elevation of the adjacent submarine rocks for the fishermen related that joints in which they had laid their crab pots beneath the water and over which they had sailed the night before with a depth of 8 or 10 feet they found to their astonishment raised far above the sea level on the next morning with their pots stranded on a reef at a height of 15 ft in the air. As the catastrophe occurred during the night no eye witnessed it but the fishermen who were out (the night being fine) were alarmed by the continual cracking of the cliff.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392812 P804496] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The strong persuasion of the neighbours connects this with the cause of the subsequent convulsion and the probable opinion is that it had forced a new channel through some of the fissures which were then opening. A fresh stream broke out after the landslip nearer the beach.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802677.jp2&y=305&x=605 Page 151]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392814 P804498] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The subsided mass pressed forward into the sea so as to approach within 100 yards of a submarine crag called the Sherborne Rock which before then was about 400 yards from the coast line. This subsidence was attended by the same phenomenon as at Culverhole and Whitelands namely the elevation of the adjacent submarine rocks for the fishermen related that joints in which they had laid their crab pots beneath the water and over which they had sailed the night before with a depth of 8 or 10 feet they found to their astonishment raised far above the sea level on the next morning with their pots stranded on a reef at a height of 15 ft in the air. As the catastrophe occurred during the night no eye witnessed it but the fishermen who were out (the night being fine) were alarmed by the continual cracking of the cliff.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392813 P804497] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The subsided mass pressed forward into the sea so as to approach within 100 yards of a submarine crag called the Sherborne Rock which before then was about 400 yards from the coast line. This subsidence was attended by the same phenomenon as at Culverhole and Whitelands namely the elevation of the adjacent submarine rocks for the fishermen related that joints in which they had laid their crab pots beneath the water and over which they had sailed the night before with a depth of 8 or 10 feet they found to their astonishment raised far above the sea level on the next morning with their pots stranded on a reef at a height of 15 ft in the air. As the catastrophe occurred during the night no eye witnessed it but the fishermen who were out (the night being fine) were alarmed by the continual cracking of the cliff.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802677.jp2&y=305&x=605 Page 151]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392815 P804499] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The subsided mass pressed forward into the sea so as to approach within 100 yards of a submarine crag called the Sherborne Rock which before then was about 400 yards from the coast line. This subsidence was attended by the same phenomenon as at Culverhole and Whitelands namely the elevation of the adjacent submarine rocks for the fishermen related that joints in which they had laid their crab pots beneath the water and over which they had sailed the night before with a depth of 8 or 10 feet they found to their astonishment raised far above the sea level on the next morning with their pots stranded on a reef at a height of 15 ft in the air. As the catastrophe occurred during the night no eye witnessed it but the fishermen who were out (the night being fine) were alarmed by the continual cracking of the cliff.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392814 P804498] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The subsided mass pressed forward into the sea so as to approach within 100 yards of a submarine crag called the Sherborne Rock which before then was about 400 yards from the coast line. This subsidence was attended by the same phenomenon as at Culverhole and Whitelands namely the elevation of the adjacent submarine rocks for the fishermen related that joints in which they had laid their crab pots beneath the water and over which they had sailed the night before with a depth of 8 or 10 feet they found to their astonishment raised far above the sea level on the next morning with their pots stranded on a reef at a height of 15 ft in the air. As the catastrophe occurred during the night no eye witnessed it but the fishermen who were out (the night being fine) were alarmed by the continual cracking of the cliff.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802677.jp2&y=305&x=605 Page 151]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392816 P804500] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The subsided mass pressed forward into the sea so as to approach within 100 yards of a submarine crag called the Sherborne Rock which before then was about 400 yards from the coast line. This subsidence was attended by the same phenomenon as at Culverhole and Whitelands namely the elevation of the adjacent submarine rocks for the fishermen related that joints in which they had laid their crab pots beneath the water and over which they had sailed the night before with a depth of 8 or 10 feet they found to their astonishment raised far above the sea level on the next morning with their pots stranded on a reef at a height of 15 ft in the air. As the catastrophe occurred during the night no eye witnessed it but the fishermen who were out (the night being fine) were alarmed by the continual cracking of the cliff.
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392815 P804499] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The subsided mass pressed forward into the sea so as to approach within 100 yards of a submarine crag called the Sherborne Rock which before then was about 400 yards from the coast line. This subsidence was attended by the same phenomenon as at Culverhole and Whitelands namely the elevation of the adjacent submarine rocks for the fishermen related that joints in which they had laid their crab pots beneath the water and over which they had sailed the night before with a depth of 8 or 10 feet they found to their astonishment raised far above the sea level on the next morning with their pots stranded on a reef at a height of 15 ft in the air. As the catastrophe occurred during the night no eye witnessed it but the fishermen who were out (the night being fine) were alarmed by the continual cracking of the cliff.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802679.jp2&y=305&x=607 Page 153]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392817 P804501] || ''Microceroceras birchii''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392816 P804500] || The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The subsided mass pressed forward into the sea so as to approach within 100 yards of a submarine crag called the Sherborne Rock which before then was about 400 yards from the coast line. This subsidence was attended by the same phenomenon as at Culverhole and Whitelands namely the elevation of the adjacent submarine rocks for the fishermen related that joints in which they had laid their crab pots beneath the water and over which they had sailed the night before with a depth of 8 or 10 feet they found to their astonishment raised far above the sea level on the next morning with their pots stranded on a reef at a height of 15 ft in the air. As the catastrophe occurred during the night no eye witnessed it but the fishermen who were out (the night being fine) were alarmed by the continual cracking of the cliff.
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802679.jp2&y=305&x=607 Page 153]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392818 P804502] || ''Androgynoceras lataecosta''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392817 P804501] || ''Microceroceras birchii''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802679.jp2&y=305&x=607 Page 153]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392819 P804503] || ''Echioceras raricostatum''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392818 P804502] || ''Androgynoceras lataecosta''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802679.jp2&y=305&x=607 Page 153]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392820 P804504] || ''Deroceras armatum''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392819 P804503] || ''Echioceras raricostatum''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802681.jp2&y=305&x=609 Page 155]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392821 P804505] || ''Amblycoceras planicosta''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392820 P804504] || ''Deroceras armatum''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802681.jp2&y=305&x=609 Page 155]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392822 P804506] || ''Amblycoceras planicosta''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392821 P804505] || ''Amblycoceras planicosta''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802681.jp2&y=305&x=609 Page 155]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392823 P804507] || ''Asteroceras oobtusum'' Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392822 P804506] || ''Amblycoceras planicosta''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802681.jp2&y=305&x=609 Page 155]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392824 P804508] || [Slab of ammonites]. [Excursion to Lyme Regis, June 2nd 1914]. [No caption].
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392823 P804507] || ''Asteroceras oobtusum'' Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802683.jp2&y=305&x=611 Page 157]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392825 P804509] || ''Oxynoticeras lymensis''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392824 P804508] || [Slab of ammonites]. [Excursion to Lyme Regis, June 2nd 1914]. [No caption].
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802683.jp2&y=305&x=611 Page 157]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392826 P804510] || ''Oxynoticeras victoris''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392825 P804509] || ''Oxynoticeras lymensis''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802683.jp2&y=305&x=611 Page 157]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392827 P804511] || ''Oxynoticeras oxynotum'', Lyme Regis. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
|-
|-
| GA002 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392826 P804510] || ''Oxynoticeras victoris''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
| [https://pubs.bgs.ac.uk/publications.html?pubID=GA002#v=d&z=2&n=5&i=P802683.jp2&y=305&x=611 Page 157]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392828 P804512] || ''Lytoceras lineatum''. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].  
|}
|}


[[Category:Geologists' Association Carreck Archive, indexes]]
[[Category:Geologists' Association Carreck Archive, indexes]]

Latest revision as of 17:09, 17 July 2020

T W Reader geological photographs, long excursions 1914. Part 2 - index, Geologists' Association 'Carreck Archive'

Link to the complete album

North Cornwall excursion, April, 1914

Page 3 P804235 Crystals of orthoclase with inclusions of biotite in St. Austell Granite, Gready Quarry. North Cornwall, April 16th 1914.
Page 3 P804236 Crystals of orthoclase with inclusions of biotite in St. Austell Granite, Gready Quarry. North Cornwall, April 16th 1914.
Page 3 P804237 Twinned crystal of orthoclase in St. Austell Granite, Gready Quarry. North Cornwall, April 16th 1914.
Page 3 P804238 Luxulyanite. North Cornwall, April 16th 1914.
Page 5 P804239 Carpalla Pit. North Cornwall, April 17th 1914. Added note: Killas.
Page 5 P804240 Carpalla Pit. North Cornwall, April 17th 1914.
Page 5 P804241 Carpalla Pit. North Cornwall, April 17th 1914. Specimens of Killas from the above section.
Page 5 P804242 Carpalla Pit. North Cornwall, April 17th 1914. Specimens of Killas from the above section. Added note: Shewing tourmalined laminae (dark) alternating with arenaceous laminae (white) in which feldspar is Kaolinised.
Page 7 P804243 Tregargus pit in China stone. North Cornwall, April 17th 1914.
Page 7 P804244 China stone with band of tourmaline. North Cornwall, April 17th 1914. Added note: Tourmaline.
Page 7 P804245 Coarsely crystallised lithium bearing Biotite in pegmatite. Trelavour Downs. North Cornwall, April 17th 1914.
Page 7 P804246 Coarsely crystallised lithium bearing biotite in pegmatite. Trelavour Downs. North Cornwall, April 17th 1914.
Page 9 P804247 Roche Rocks. North Cornwall, April 17th 1914.
Page 9 P804248 Roche Rocks. North Cornwall, April 17th 1914.
Page 9 P804249 Roche Rocks. North Cornwall, April 17th 1914.
Page 9 P804250 Roche Rocks. North Cornwall, April 17th 1914.

Excursion to Derbyshire, July, 1914

Page 13 P804251 Black Rocks - Cromford. Millstone Grit Escarpment. Excursion to Derbyshire, July 28th 1914. [People].
Page 13 P804252 Black Rocks - Cromford. Millstone Grit Escarpment. Excursion to Derbyshire, July 28th 1914.
Page 13 P804253 In Derbyshire the Millstone Grit is made up of five thick beds of Sandstone each divided by a series of shales and sands interbedded. Excursion to Derbyshire, July 28th 1914. These 'Black Rocks' belong to the Fourth or Upper Kinder Scout Grit which here forms an escarpment. The rock standing out as bold craggy cliffs from the surrounding slopes and weathered into various shapes this having the fantastic title of the 'Field Gun'.
Page 13 P804254 In Derbyshire the Millstone Grit is made up of five thick beds of Sandstone each divided by a series of shales and sands interbedded. Excursion to Derbyshire, July 28th 1914. These 'Black Rocks' belong to the Fourth or Upper Kinder Scout Grit which here forms an escarpment. The rock standing out as bold craggy cliffs from the surrounding slopes and weathered into various shapes this having the fantastic title of the 'Field Gun'.
Page 15 P804255 Dolomitized Mountain Limestone - Hopton Wood Quarry by Middleton. This stone was largely used in building the Imperial Institute. Derbyshire, July 28th 1914.
Page 15 P804256 Dolomitized Mountain Limestone - Hopton Wood Quarry by Middleton. This stone was largely used in building the Imperial Institute. Derbyshire, July 28th 1914.
Page 17 P804257 Section in the Dolerite Sill at Ible. Derbyshire, July 28th 1914.
Page 17 P804258 [Ible]. Derbyshire, July 28th 1914. These igneous rocks of Derbyshire go by the name of Toadstones. Some say because the amydaloidal parts resemble the back of a toad while others trace it to the German word Todstein meaning dead stone because no ore is found in it.
Page 17 P804259 This sill at Ible is one of nine intrusions of igneous material in this part of Derbyshire. Derbyshire, July 28th 1914.
Page 17 P804260 [Ible]. Derbyshire, July 28th 1914. In the centre of the intrusion the dolerite is coarse grained and ophitic but at the margins it is very finegrained. [People].
Page 19 P804261 This sheet or sill of intrusive dolerite has a thickness of about 70 feet and is quarried for road metal. The Limestone below it has been baked into marble for a depth of several feet. Derbyshire, July 28th 1914. [People].
Page 19 P804262 This sheet or sill of intrusive dolerite has a thickness of about 70 feet and is quarried for road metal. The Limestone below it has been baked into marble for a depth of several feet. Derbyshire, July 28th 1914.
Page 19 P804263 Joints in dolerite caused by shrinkage and disturbance. Derbyshire, July 28th 1914.
Page 19 P804264 Vein of Chrysolite in Dolerite Sill. Ible. Wirksworth. Derbyshire, July 28th 1914. These veins of chrysolite are found traversing the dolerite. The mineral is of a golden yellow colour and is built up of prisms or bundles of parallel fibres arranged perpendicularly to the walls of the cracks in which it has been deposited.
Page 21 P804265 [Grange Mill]. Derbyshire, July 28th 1914. Shothouse Spring. nodular and concretionary limestone resting on a bed of laminated tuff. To a height of about 10 ft above the spring the limestone is found to contain numerous small lapilli.
Page 21 P804267 Agglomerate at Grange Mill which was formerly a volcanic vent. This weathers into spheroids as seen above which were exposed in the southern vent. Derbyshire, July 28th 1914.
Page 21 P804268 Agglomerate at Grange Mill which was formerly a volcanic vent. This weathers into spheroids as seen above which were exposed in the southern vent. Derbyshire, July 28th 1914.
Page 23 P804269 Tufa Quarry, Via Gellia. This tufa consists of an amorphous carbonate of lime which has been deposited from a waterfall which previously existed at this place. Derbyshire, July 28th 1914. [Person].
Page 23 P804270 Tufa Quarry, Via Gellia. This tufa consists of an amorphous carbonate of lime which has been deposited from a waterfall which previously existed at this place. Derbyshire, July 28th 1914. [Person].
Page 23 P804271 [Via Gellia]. Derbyshire, July 28th 1914. The present stream and waterfall as now existing by the side of the quarry shown above.
Page 23 P804272 [Via Gellia]. Derbyshire, July 28th 1914. The present stream and waterfall as now existing by the side of the quarry shown above.
Page 25 P804273 Scrablag. A local name for peculiarly shaped concretions in sand. Ible. Derbyshire, July 28th 1914.
Page 25 P804274 Scrablag. Ible Sill. Derbyshire, July 28th 1914.
Page 25 P804275 Tufa. Via Gellia. Matlock Bath. Derbyshire, July 28th 1914. The Tufa is deposited around twigs, leaves, moss, shells, and bones of animals.
Page 25 P804276 Tufa. With Helix. Matlock Bath. Derbyshire, July 28th 1914. The Tufa is deposited around twigs, leaves, moss, shells, and bones of animals.
Page 27 P804277 Carboniferous Limestone, Via Gellia. The smooth surface on the right is considered by some to be slickensided. Derbyshire, July 28th 1914. [People].
Page 27 P804278 Spheroidal dolerite, Via Gellia. Derbyshire, July 28th 1914.
Page 27 P804279 Quarry in spheroidal dolerite near the Paint Works, Via Gellia. Derbyshire, July 28th 1914.
Page 27 P804280 Quarry in spheroidal dolerite near the Paint Works, Via Gellia. Derbyshire, July 28th 1914.
Page 29 P804281 Spheroidal dolerite in quarry near Pig of Lead, Matlock Bath. Derbyshire, July 28th 1914.
Page 29 P804282 Spheroidal dolerite in quarry near Pig of Lead, Matlock Bath. Derbyshire, July 28th 1914.
Page 29 P804283 Spheroidal dolerite in quarry near Pig of Lead, Matlock Bath. Derbyshire, July 28th 1914.
Page 29 P804284 Spheroidal dolerite in quarry near Pig of Lead, Matlock Bath. Derbyshire, July 28th 1914.
Page 31 P804285 Ravenstor, Millers Dale. Derbyshire, July 29th 1914.
Page 31 P804286 Ravenstor, Millers Dale. Derbyshire, July 29th 1914. Carboniferous Limestone resting on Lower Lava.
Page 31 P804287 Ravenstor, Millers Dale. Derbyshire, July 29th 1914. In Tarnsley Dale. [Group photo].
Page 31 P804288 Ravenstor, Millers Dale. Derbyshire, July 29th 1914. Tideswell Dale.
Page 33 P804289 Derbyshire, July 29th 1914. [Group photo, large version].
Page 35 P804290 Derbyshire County Council Pit, Tideswell Dale. Derbyshire, July 29th 1914. This dolerite which is worked for road metal is found in a sill which has a thickness of about 70 feet. It extends for nearly half a mile in a North to South direction. [People].
Page 35 P804291 Derbyshire County Council Pit, Tideswell Dale. Derbyshire, July 29th 1914. The dolerite varies in structure, in the centre it is coarsely crystalline while at the upper and lower surfaces it is fine grained. [People].
Page 35 P804292 Derbyshire County Council Pit, Tideswell Dale. Derbyshire, July 29th 1914. Spheroidal weathering.
Page 35 P804293 Derbyshire County Council Pit, Tideswell Dale. Derbyshire, July 29th 1914. Spheroidal weathering.
Page 37 P804294 Columnar Volcanic Mud. Baked by Lava Flow. Tideswell Dale. Derbyshire, July 29th 1914. At Tideswell Dale is a bed of red clay which was formerly a volcanic mud. This is found interbedded in the limestone. After its deposition a stream of lava flowed over it which hardened and baked it and caused it to assume a columnar structure.
Page 37 P804295 Columnar Volcanic Mud. Baked by Lava Flow. Tideswell Dale. Derbyshire, July 29th 1914. At Tideswell Dale is a bed of red clay which was formerly a volcanic mud. This is found interbedded in the limestone. After its deposition a stream of lava flowed over it which hardened and baked it and caused it to assume a columnar structure.
Page 37 P804296 Carboniferous limestone, Monsal Dale. Derbyshire, July 29th 1914.
Page 37 P804297 Spheroides of Dolerite. Tideswell Dale. Derbyshire, July 29th 1914. Owing to a chemical change in the dolerite due to weathering the blocks assume a spheroidal form.
Page 39 P804298 Peep o' Day Quarry in the Carboniferous Limestone at Litton. This was originally a coral reef but is now consolidated into a hard massive limestone. Derbyshire, July 29th 1914.
Page 39 P804299 Peep o' Day Quarry in the Carboniferous Limestone at Litton. This was originally a coral reef but is now consolidated into a hard massive limestone. Derbyshire, July 29th 1914.
Page 39 P804300 [Peep o' Day Quary]. Derbyshire, July 29th 1914. Owing to the action of the weather on the exposed surfaces of the limestones the fine coral mud is gradually worn away leaving the corals standing out in relief in the positions in which they lived. Added note: coral.
Page 39 P804301 [Peep o' Day Quary]. Derbyshire, July 29th 1914. Owing to the action of the weather on the exposed surfaces of the limestones the fine coral mud is gradually worn away leaving the corals standing out in relief in the positions in which they lived. Added note: coral.
Page 41 P804302 Stepping stones across bed of what is a mountain torrent after rain. Cressbrook Dale. Derbyshire, July 29th 1914.
Page 41 P804303 [Cressbrook Dale]. Derbyshire, July 29th 1914.
Page 41 P804304 [Cressbrook Dale]. Derbyshire, July 29th 1914. Cressbrook Mill Stream! In dry weather this is a dry river bed in the Carboniferous limestone but after rain it becomes a mountain torrent. It shows the angular blocks being formed into pebbles.
Page 41 P804305 [Cressbrook Dale]. Derbyshire, July 29th 1914. Cressbrook Mill Stream! In dry weather this is a dry river bed in the Carboniferous limestone but after rain it becomes a mountain torrent. It shows the angular blocks being formed into pebbles.
Page 43 P804306 Derbyshire, July 29th 1914.
Page 43 P804307 Derbyshire, July 29th 1914.
Page 43 P804308 River Wye at Monsal Dale (Headstones). Derbyshire, July 29th 1914. The River Wye generally described as 'a singularly romantic river, running in deep rocky ravines, its clear stream sparkling along a confined and rugged bed' rises near Buxton on the northern slope of Axe Edge and joins the Derwent at Rowsley.
Page 43 P804309 River Wye at Monsal Dale (Headstones). Derbyshire, July 29th 1914. The River Wye generally described as 'a singularly romantic river, running in deep rocky ravines, its clear stream sparkling along a confined and rugged bed' rises near Buxton on the northern slope of Axe Edge and joins the Derwent at Rowsley.
Page 45 P804310 Boulder Clay overlying Carboniferous Limestone, Monsal Dale Station Quarry. Derbyshire, July 29th 1914. Some of the boulders consist of rock derived from the immediate locality while others have travelled from great distances, they are much scratched grooved and polished.
Page 45 P804311 Boulder Clay overlying Carboniferous Limestone, Monsal Dale Station Quarry. Derbyshire, July 29th 1914. Some of the boulders consist of rock derived from the immediate locality while others have travelled from great distances, they are much scratched grooved and polished. [People].
Page 45 P804312 Slickensided Carboniferous Limestone caused by one face of the rock sliding over the other owing to earth movements. Derbyshire, July 29th 1914.
Page 45 P804313 Calc spar mine, Monsal Dale. This mine for obtaining calc spar is driven into a rake vein about 2 feet in width in the Carboniferous limestone. The vein is filled with calc spar with galena and barytes. Derbyshire, July 29th 1914.
Page 47 P804314 Ridgeway Cutting, Ambergate. Derbyshire, July 30th 1914. Overthrust Fault in Coal seam, locally known as the 'Norton' seam.
Page 47 P804315 Ridgeway Cutting, Ambergate. Derbyshire, July 30th 1914. Lower Coal Measures, Ridgeway Ry [Railway] Cutting.
Page 47 P804316 Ridgeway Cutting, Ambergate. Derbyshire, July 30th 1914. Coal seam, 'Norton' Seam. [Person].
Page 47 P804317 Ridgeway Cutting, Ambergate. Derbyshire, July 30th 1914. Lower Coal Measures in Ridgeway Cutting. Added note: 4=shales, 3=Gannister, 2=White Snady Fine Clay, 1=Sandstone.
Page 49 P804318 Ridgeway Quarry in Millstone Grit. The Topmost Grit or 'Rough Rock'. Derbyshire, July 30th 1914.
Page 49 P804319 Bullbridge Brickyard Pit in the Lower Coal Measures. Derbyshire, July 30th 1914. Added note: Shale resting on Marine Band above Alton Seam.
Page 49 P804320 The Alton Coal seam Bullbridge Brickyard. This coal seam is about 300 feet above the base of the Coal Measures and is correlated with the Crabtree Coal of North Staffordshire and the Bullion Coal of Lancashire. Derbyshire, July 30th 1914. [Person].
Page 49 P804321 The Alton Coal seam Bullbridge Brickyard. This coal seam is about 300 feet above the base of the Coal Measures and is correlated with the Crabtree Coal of North Staffordshire and the Bullion Coal of Lancashire. Derbyshire, July 30th 1914. [Person].
Page 51 P804322 Crich. Derbyshire, July 30th 1914. This inlier consists of a mass of Carboniferous Limestone about 1.5 miles in length. It forms an elongated dome running from N.N.W. to S.S.E.
Page 51 P804323 Crich. Derbyshire, July 30th 1914. This tower known as Crich Stand is built on the summit of a mass of Carboniferous Limestone known as the Crich inlier. It is 940 feet above sea level.
Page 51 P804324 Crich. Derbyshire, July 30th 1914. Mammilated surface of Limestone. Cliff Quarry, Crich.
Page 51 P804325 Crich. Derbyshire, July 30th 1914. Cliff Quarry in the Crich inlier Carb. [Carboniferous] Limestone. This is D2. of Dr Vaughan. The limestone is traversed with viens containing Calcite, Fluorite, barytes, galena and Blendes. [People].
Page 53 P804326 The Old Quarry in Carboniferous Limestone, Crich. The Limestone is capped by Glacial Drift containing local and foreign erratics. Derbyshire, July 30th 1914.
Page 53 P804327 The Old Quarry in Carboniferous Limestone, Crich. The Limestone is capped by Glacial Drift containing local and foreign erratics. Derbyshire, July 30th 1914.
Page 53 P804328 [Old Quarry, Crich]. Derbyshire, July 30th 1914. 'Pothole'. Solution-cavities in limestone filled with clay.
Page 53 P804329 The Old Quarry, Crich. Solution cavities in Carb. [Carboniferous] Limestone filled with clay. Derbyshire, July 30th 1914.
Page 55 P804330 Hilt's Quarry, Crich. Carboniferous Limestone. Derbyshire, July 30th 1914.
Page 55 P804331 Hilt's Quarry, Crich. Carboniferous Limestone. Derbyshire, July 30th 1914.
Page 57 P804332 Howden Dam. Derbyshire, July 31st 1914.
Page 57 P804333 Anticline in shales and sandstones on river bank below Howden Dam. Derbyshire, July 31st 1914.
Page 57 P804334 Anticline in shales and sandstones on river bank below Howden Dam. Derbyshire, July 31st 1914.
Page 59 P804335 Darley Dale Quarry. Derbyshire, August 1st 1914. The Mountain Limestone forms in Derbyshire an inlier of an irregular shape stretching 20 miles from North to South and above 10 miles from East to West with a few little patches in other localities. Owing to earth movements this large inlier forms a pericline or dome, the beds dipping away from the middle of the dome in every direction.
Page 59 P804336 Darley Dale Quarry. Derbyshire, August 1st 1914. The Mountain Limestone forms in Derbyshire an inlier of an irregular shape stretching 20 miles from North to South and above 10 miles from East to West with a few little patches in other localities. Owing to earth movements this large inlier forms a pericline or dome, the beds dipping away from the middle of the dome in every direction.
Page 59 P804337 Darley Dale Quarry. Derbyshire, August 1st 1914. On examination it appears that some of the layers had their origin from reef like accumulations very much like those in the Pacific coral islands and shell banks while others were more fragmental and made up of broken corals, crinoid stems and shells which the waves had spread over the sea bottom.
Page 59 P804338 Darley Dale Quarry. Derbyshire, August 1st 1914. On examination it appears that some of the layers had their origin from reef like accumulations very much like those in the Pacific coral islands and shell banks while others were more fragmental and made up of broken corals, crinoid stems and shells which the waves had spread over the sea bottom. Added note: Crinoidal limestone beds.
Page 61 P804339 Dolomitized limestone or Dunstone showing the typical weathering into castellated masses at Wyn's Tor above Winster. Derbyshire, August 1st 1914. [Group photo].
Page 61 P804340 Dolomitized limestone or Dunstone showing the typical weathering into castellated masses at Wyn's Tor above Winster. Derbyshire, August 1st 1914.
Page 61 P804341 Chert quarry, Winster. Derbyshire, August 1st 1914. This chert is a silicious limestone which is sent to the Staffordshire potteries for making china and porcelain. Owing to its crystalline structure it differs from the nodules and layers of chert which are found in the upper beds of the Mountain limestone. [People].
Page 61 P804342 Chert quarry, Winster. Derbyshire, August 1st 1914. This chert is a silicious limestone which is sent to the Staffordshire potteries for making china and porcelain. Owing to its crystalline structure it differs from the nodules and layers of chert which are found in the upper beds of the Mountain limestone. [People].
Page 63 P804343 Robin Hoods Stride or Mock Beggars Hall in the Fourth or Upper Kinder Scout Grit of the Millstone Grit. Derbyshire, August 1st 1914. The stride which Robin Hood must have taken to get the place named after him, that is, the distance from these two turrets is about 10 to 15 yards. [People].
Page 63 P804344 Robin Hoods Stride or Mock Beggars Hall in the Fourth or Upper Kinder Scout Grit of the Millstone Grit. Derbyshire, August 1st 1914. The stride which Robin Hood must have taken to get the place named after him, that is, the distance from these two turrets is about 10 to 15 yards. [People].
Page 63 P804345 Cone-In-Cone. Bullbridge Ambergate. Derbyshire, August 1st 1914.
Page 65 P804346 The Dakin Valley, Alport, showing the thick horizontal beds of Carboniferous limestone. It is from these 'Scars' which are bare precipices or mural escarpments that Sedgwick named this the 'Scar limestone'. Derbyshire, August 1st 1914. [People].
Page 65 P804347 The Dakin Valley, Alport, showing the thick horizontal beds of Carboniferous limestone. It is from these 'Scars' which are bare precipices or mural escarpments that Sedgwick named this the 'Scar Limestone'. Derbyshire, August 1st 1914.
Page 65 P804348 [Joints]. Derbyshire, August 1st 1914. In these scars are frequently seen joints like the above which are formed by shrinkage and sometimes by disturbance. These cracks which are generally at right angles to the bedding are gradually enlanged by the action of water.
Page 65 P804349 Tufa Quarry, Alport. This creamy white rock is formed by the deposition of lime from calcareous springs and is of variable texture, in places being hard and crystalline and in others soft, friable and cellular. Derbyshire, August 1st 1914. [Person].
Page 67 P804350 Old Mill Quarry,Stanton Mill. The Black Shales of the Pendleside Series containing Posidoniella laevis are here seen to rest with unconformity on the limestones of the Lonsdalia subzone. Derbyshire, August 1st 1914. The shales which show no signs of disturbance rest evenly upon a surface formed by the truncated edges of the limestone beds. This shows the commencement of an anticlinal dome of limestone. If stripped of the shale above, the dome would have a knoll like aspect thus indicating contemporaneous elevation and erosion causing local unconformity. Added note: Grey limestones with strong chert, Carboniferous Limestone, Lonsdalia sub-zone. Black Shales, Pendleside Series.
Page 67 P804351 Old Mill Quarry,Stanton Mill. The Black Shales of the Pendleside Series containing Posidoniella laevis are here seen to rest with unconformity on the Limestones of the Lonsdalia subzone. Derbyshire, August 1st 1914. The shales which show no signs of disturbance rest evenly upon a surface formed by the truncated edges of the limestone beds. This shows the commencement of an anticlinal dome of Limestone. If stripped of the shale above, the dome would have a knoll like aspect thus indicating contemporaneous elevation and erosion causing local unconformity. Added note: Limestone, Black Shales. [People].
Page 67 P804352 Old Mill Quarry,Stanton Mill. The Black Shales of the Pendleside Series containing Posidoniella laevis are here seen to rest with unconformity on the Limestones of the Lonsdalia subzone. Derbyshire, August 1st 1914. The shales which show no signs of disturbance rest evenly upon a surface formed by the truncated edges of the limestone beds. This shows the commencement of an anticlinal dome of Limestone. If stripped of the shale above, the dome would have a knoll like aspect thus indicating contemporaneous elevation and erosion causing local unconformity.
Page 67 P804353 River Dakin - Alport. This is an interesting case of a calcareous stream forming terraces of travertine or tufa. The calcium carbonate being thrown down in ridges or terraces by the escape of carbonic acid and evaporation. Derbyshire, August 1st 1914.
Page 69 P804354 Harboro' [Harborough] pit, Brassington. Derbyshire, August 2nd 1914. These deposits of brightly coloured sands and clays in various shades of red and yellow with white are found in large irregular hollows in the Carboniferous Limestone occurring between Hartington and Brassington in a N.W. to S.E. direction. These hollows which are sometimes 100 yards across are thought to be swallow holes filled in with fine clay and clean sand with white and red quartzite pebbles. Their age is uncertain - they are evidently preglacial and some go so far as to consider them of Bunter age. The materials have the character of a broken up Kinder Scout Grit and the sands and pebbles agree with the Bunter Beds. The clay obtained here is used by the Derby Porcelain works. [Caption of two photos combined as form continuous text].
Page 69 P804355 Harboro' [Harborough] pit, Brassington. Derbyshire, August 2nd 1914. These deposits of brightly coloured sands and clays in various shades of red and yellow with white are found in large irregular hollows in the Carboniferous Limestone occurring between Hartington and Brassington in a N.W. to S.E. direction. These hollows which are sometimes 100 yards across are thought to be swallow holes filled in with fine clay and clean sand with white and red quartzite pebbles. Their age is uncertain - they are evidently preglacial and some go so far as to consider them of Bunter age. The materials have the character of a broken up Kinder Scout Grit and the sands and pebbles agree with the Bunter Beds. The clay obtained here is used by the Derby Porcelain works. [Caption of two photos combined as form continuous text].
Page 71 P804356 Carboniferous Limestone, Cromford. Derbyshire, August 3rd 1914.
Page 71 P804357 Cromford Quarry. Derbyshire, August 3rd 1914. [Person].
Page 71 P804358 Bonsall. Derbyshire, August 3rd 1914. [Group photo].
Page 71 P804359 Quartzose Limestone, Bonsall. Derbyshire, August 3rd 1914.
Page 73 P804360 [Bonsall]. Derbyshire, August 3rd 1914. [Group photo - large version of previous].
Page 75 P804361 Quarry in Spheroidal Dolerite - Pot Luck Farm (Drabble's Quarry), Bonsall. Derbyshire, August 3rd 1914. When the Carboniferous limestone had assumed its solid condition masses of molten matter were forced up from the interior of the Earth in some places crossing the beds and in others pushing between them now forming hard rock suitable for road metal. [People].
Page 75 P804362 Quarry in spheroidal dolerite - Pot Luck Farm (Drabble's Quarry), Bonsall. Derbyshire, August 3rd 1914. When the Carboniferous limestone had assumed its solid condition masses of molten matter were forced up from the interior of the Earth in some places crossing the beds and in others pushing between them now forming hard rock suitable for road metal. [People].
Page 75 P804363 ??????. Derbyshire, August 3rd 1914. In the process of cooling and contraction this rock frequently assumes a columnar structure and often divided by cross joints. In this case instead of being angular each segment owing to weathering takes a spheroidal form. It is stated that the cause of this is owing to the middle of each spheroid being a centre of crystallisation around which the different minerals of the rock arranged themselves.
Page 75 P804364 ???????. Derbyshire, August 3rd 1914. In the process of cooling and contraction this rock frequently assumes a columnar structure and often divided by cross joints. In this case instead of being angular each segment owing to weathering takes a spheroidal form. It is stated that the cause of this is owing to the middle of each spheroid being a centre of crystallisation around which the different minerals of the rock arranged themselves.
Page 77 P804365 The valley of the Derwent from near Masson Hill looking along Darley Dale. Derbyshire, August 3rd 1914.
Page 77 P804366 Limestone quarry, Matlock Bridge. This is in thinly bedded cherty limestones and contains fossils that show that it is of the subzone known as D3. Derbyshire, August 3rd 1914.
Page 77 P804367 The High Tor and Gorge of the Derwent through the Mountain Limestone which extends as far as Willersley when the river then winds through more open valleys to Derby and thence on to the Trent. Derbyshire, August 3rd 1914.
Page 79 P804368 Tufa Quarry, Matlock Bath. The circular holes were originally branches of trees coated by tufa. In course of time the wood decayed thus leaving spaces like pipes. Derbyshire, August 3rd 1914.
Page 79 P804369 The more solid pieces are used for building purposes, but the porous portions are only fit for rock gardens. Derbyshire, August 3rd 1914.
Page 79 P804370 Tufa. Matlock Bath. Derbyshire, August 3rd 1914. A mass of twigs coated with tufa from the above quarry.
Page 81 P804371 Tufa. Matlock Bath. Derbyshire, August 3rd 1914. Tufa which also goes by the name of travertin [travertine] or calcareous sinter is a deposit of carbonate of lime thrown down by springs which flow through beds of limestone. In this case at Matlock these specimens are from lime obtained from the Carboniferous limestone. The rain in passing through the atmosphere takes up Carbonic acid and assisted by humic acid from the soil when it sinks into the limestone dissolves portions of it away. When it comes to the surface again in the form of springs it loses some of the carbonic acid and the lime is thrown down in the form of tufa and incrusting any object that happens to be present.
Page 81 P804372 Tufa. Matlock Bath. Derbyshire, August 3rd 1914. Tufa which also goes by the name of travertin [travertine] or calcareous sinter is a deposit of carbonate of lime thrown down by springs which flow through beds of limestone. In this case at Matlock these specimens are from lime obtained from the Carboniferous limestone. The rain in passing through the atmosphere takes up Carbonic acid and assisted by humic acid from the soil when it sinks into the limestone dissolves portions of it away. When it comes to the surface again in the form of springs it loses some of the carbonic acid and the lime is thrown down in the form of tufa and incrusting any object that happens to be present.
Page 81 P804373 Tufa. Matlock Bath. Derbyshire, August 3rd 1914. Tufa which also goes by the name of Travertin [Travertine] or Calcareous Sinter is a deposit of Carbonate of Lime thrown down by springs which flow through beds of limestone. In this case at Matlock these specimens are from lime obtained from the Carboniferous limestone. The rain in passing through the atmosphere takes up Carbonic acid and assisted by humic acid from the soil when it sinks into the limestone dissolves portions of it away. When it comes to the surface again in the form of springs it loses some of the carbonic acid and the lime is thrown down in the form of tufa and incrusting any object that happens to be present.
Page 81 P804374 Tufa which also goes by the name of travertin [travertine] or calcareous sinter is a deposit of carbonate of lime thrown down by springs which flow through beds of limestone. Derbyshire, August 3rd 1914. In this case at Matlock these specimens are from lime obtained from the Carboniferous limestone. The rain in passing through the atmosphere takes up Carbonic acid and assisted by humic acid from the soil when it sinks into the limestone dissolves portions of it away. When it comes to the surface again in the form of springs it loses some of the carbonic acid and the lime is thrown down in the form of tufa and incrusting any object that happens to be present.
Page 83 P804375 Carlton Hill Vent. Derbyshire, August 4th 1914. The volcanoes from which the Derbyshire Toadstone was thrown out have long been buried under later deposits on the sea bottom but in places where these deposits have been cleared away were are able to see the necks or pipes through which the molten lava was forced up. Carlton Hill is one of these necks filled with Agglomerate and Basalt containing olivine nodules. [People].
Page 83 P804376 Carlton Hill Vent. Derbyshire, August 4th 1914. The volcanoes from which the Derbyshire Toadstone was thrown out have long been buried under later deposits on the sea bottom but in places where these deposits have been cleared away were are able to see the necks or pipes through which the molten lava was forced up. Carlton Hill is one of these necks filled with Agglomerate and Basalt containing olivine nodules. [Person].
Page 83 P804377 Owing to the combined result of crystallization and cooling causing contraction the Basalt weathers into a mass of rough spheroides. Derbyshire, August 4th 1914.
Page 83 P804378 The Gorge of the River Wye through Carboniferous Limestone. Derbyshire, August 4th 1914.
Page 85 P804379 Upper Lava resting on Carboniferous Limestone at Knott [Knot] Low, Millers Dale. Derbyshire, August 4th 1914. [People].
Page 85 P804380 Upper Lava resting on Carboniferous Limestone at Knott [Knot] Low, Millers Dale. Derbyshire, August 4th 1914.
Page 85 P804381 Ice-Scratched Boulder. Boulder Clay. Alport. Rowsley. Derbyshire, August 4th 1914.

Excursion to Lyme Regis, May-June, 1914

Page 89 P804382 Lyme Regis looking West. Excursion to Lyme Regis, May 30th 1914. The town is built on the clayey portion of the Lias which is seen in the upper part of its cliffs. The limestones or Blue Lias are not seen in the town being bent downwards in the trough of a synclinal curve which bends the beds down to sea level.
Page 89 P804383 Lyme Regis looking West. Excursion to Lyme Regis, May 30th 1914. The town is built on the clayey portion of the Lias which is seen in the upper part of its cliffs. The limestones or Blue Lias are not seen in the town being bent downwards in the trough of a synclinal curve which bends the beds down to sea level.
Page 89 P804384 Looking East from just west of the Cobb. The cliffs in the distance are , on the left Stonebarrow, the high one in the centre is Golden Cap with Thorncombe Beacon beyond. Excursion to Lyme Regis, May 30th 1914.
Page 89 P804385 The Harbour of Lyme known as the Cobb. This is built of Cowstones within and faced with Portland Roach. Excursion to Lyme Regis, May 30th 1914.
Page 91 P804386 Church Cliffs - Lyme Regis. Excursion to Lyme Regis, May 30th 1914. Looking N.E. from point about 290 yards N.E. of Lyme Church. Added note: Table Ledge, Glass Bottle, Top Q. [Quick], Verity, Best, 2nd and Rattle, Mid Quick.
Page 91 P804387 Church Cliffs - Lyme Regis. Excursion to Lyme Regis, May 30th 1914. Looking N.W. from a point about 420 yards N.E. of Lyme Church. Added note: Grey, Glass Bottle, Top Quick, Verity, Best, Second, Rattle, Mid Quick, Gumption, 3rd Quick, Top Tape, 2nd Tape, Top Copper, Mongrel, 2nd Mongrel, Specketty.
Page 91 P804388 Church Cliffs - Lyme Regis. Excursion to Lyme Regis, May 30th 1914. Church Cliffs at about 360 yards N.E. of Lyme Church. Added note: Fish, Grey, Glass Bottle, Top Quick, Verity, Best, Second, Ratt [Rattle], M. Quick, Gumption, 3rd Quick, Top Tape, 2nd Tape, Top Copper, Mongrel.
Page 91 P804389 Church Cliffs - Lyme Regis. Excursion to Lyme Regis, May 30th 1914. Church Cliffs at about 220 yards N.E. of Lyme Church. Added note: Top Quick, Verity, Best, Second, Rattle, Mid Quick, Gumption.
Page 93 P804390 Fault at Church Cliffs at about 260 yards N.E. of Lyme Church. Excursion to Lyme Regis, May 30th 1914. Added note: Grey Ledge, Glass Bottle, Top Quick, Verity, Best Bed, Second Bed, Rattle, Middle Quick, Gumption.
Page 93 P804391 A view of Church Cliffs from very close to Lyme about 120 yards East of Lyme Church. Excursion to Lyme Regis, May 30th 1914. Added note: Grey Ledge, Glass Bottle, Top Quick, Verity, Best, 2nd Bed, Rattle.
Page 93 P804392 Fault in centre of photograph. The downthrow is on the west or left hand side. Excursion to Lyme Regis, May 30th 1914. Added note: Glass Bottle, Top Quick, Verity, Best, 2nd, Rattle, Mid Quick, Gumption, Third Quick.
Page 93 P804393 5/8 of a mile N.W. of Lyme Church. This is on the western limb of the Church Cliffs Anticline and represents a local disturbance with slight faulting of the bedding. Excursion to Lyme Regis, May 30th 1914. Added note: Glass Bottle, Best, 2nd, Rattle, Mid Quick, Gumption, Third Quick. [People].
Page 95 P804394 The Burning Mound. This is composed of shales, iron pyrites and cement stones. Excursion to Lyme Regis, May 30th 1914. This so called 'volcano' took fire in 1908. Rapid decomposition of the iron pyrites induced by a particularly wet season acting on clay with much inflammable (butuminous) matter in its composition is supposed to account for the phenomenon. Added note: About 1/2 mile N.E. of Lyme Church.
Page 95 P804395 The Burning Mound. This is composed of Shales, iron pyrites and cement stones. Excursion to Lyme Regis, May 30th 1914. This so called 'volcano' took fire in 1908. Rapid decomposition of the Iron Pyrites induced by a particularly wet season acting on clay with much inflammable (butuminous) matter in its composition is supposed to account for the phenomenon. Added note: About 1/2 mile N.E. of Lyme Church.
Page 95 P804396 Pieces of baked shale showing discolouration in concentric rings according to different degrees of burning. Excursion to Lyme Regis, May 30th 1914.
Page 95 P804397 Pieces of baked shale showing discolouration in concentric rings according to different degrees of burning. Excursion to Lyme Regis, May 30th 1914.
Page 97 P804398 General view of the Cliffs and Coast looking East from about 3/4 mile N.E. of Lyme Church. Excursion to Lyme Regis, May 30th 1914.
Page 97 P804399 General view of the cliffs and coast looking East from about 3/4 mile N.E. Of Lyme Church. Excursion to Lyme Regis, May 30th 1914. Added note: Bel. [Belemnite] Marls, Stellaris Beds.
Page 97 P804400 The face of Black Ven at about 800 yards West of the end of Lower Sea Lane. Charmouth Beach and just east of Black Ven Rocks. Excursion to Lyme Regis, May 30th 1914. Added note: Stellaris Beds, Birchi Bed.
Page 97 P804401 The face of Black Ven at about 800 yards West of the end of Lower Sea Lane. Charmouth Beach and just east of Black Ven Rocks. Excursion to Lyme Regis, May 30th 1914.
Page 99 P804402 Black Ven looking in a N.E. direction from between Canary Ledges and Cockpits about 5/8 of a mile west of Charmouth Beach. Excursion to Lyme Regis, May 30th 1914.
Page 99 P804403 Black Ven looking in a N.E. direction from between Canary Ledges and Cockpits about 5/8 of a mile west of Charmouth Beach. Excursion to Lyme Regis, May 30th 1914.
Page 99 P804404 Black Ven from the beach at Cockpits. Excursion to Lyme Regis, May 30th 1914. [Person].
Page 101 P804405 Fault in the 'Shales-with-Beef' below the Birchi Bed. 'Beef' is a fibrous calcium carbonate. Excursion to Lyme Regis, May 30th 1914.
Page 101 P804406 An undulation accompanying a fault in the Shales-with-Beef. The strings of Beef vary in thickness from a fraction of an inch up to 2 or 3 inches. Even when extremely thin they are nearly always double. Excursion to Lyme Regis, May 30th 1914.
Page 101 P804407 Limestone nodule in Shales with Beef. These nodules often occur in connection with the Beef strings. When this occurs the two halves of the beef string diverge and the nodule lies between the enwrapping layers. Excursion to Lyme Regis, May 30th 1914.
Page 103 P804408 White Lias (Rhaetic beds) and Blue Lias Limestones and Shales at Pinhay Bay. Excursion to Lyme Regis, May 31st 1914. The lower beds of the Rhaetic, the Black Avicular contorta shales can be seen at low tide on the foreshore but the Cotham Marble is not exposed owing no doubt to its coverings of beach shingle and boulders. It has however been observed at Charton Bay.
Page 103 P804409 White Lias (Rhaetic beds) and Blue Lias Limestones and Shales at Pinhay Bay. Excursion to Lyme Regis, May 31st 1914. The lower beds of the Rhaetic, the Black Avicular contorta shales can be seen at low tide on the foreshore but the Cotham Marble is not exposed owing no doubt to its coverings of beach shingle and boulders. It has however been observed at Charton Bay.
Page 103 P804410 The Rhaetic Beds . Excursion to Lyme Regis, May 31st 1914. The Rhaetic Beds mark the commencement of the physical changes which terminated the continental conditions of the Trias and ushered in the marine conditions of the Jurassic, changes that evidently were not brought about uniformly over the British area. Added note: White Lias.
Page 103 P804411 The Rhaetic Beds . Excursion to Lyme Regis, May 31st 1914. The Rhaetic Beds mark the commencement of the physical changes which terminated the continental conditions of the Trias and ushered in the marine conditions of the Jurassic, changes that evidently were not brought about uniformly over the British area. Added note: Lias, White Lias or Rhaetic, Black shales.
Page 105 P804412 The White Lias is a white or cream coloured limestone hard and smooth grained in the lowest beds. Excursion to Lyme Regis, May 31st 1914. Some of the more marly beds contain pebble like concretions composed of limestone similar to the white limestone. These stand out on the weathered surface of the rock in small lumps and impart to it a comglomerate appearance.
Page 105 P804413 The White Lias is a white or cream coloured limestone hard and smooth grained in the lowest beds. Excursion to Lyme Regis, May 31st 1914. Some of the more marly beds contain pebble like concretions composed of limestone similar to the white limestone. These stand out on the weathered surface of the rock in small lumps and impart to it a comglomerate appearance. Added note: White Lias. [Person].
Page 105 P804414 The White Lias is a white or cream coloured limestone hard and smooth grained in the lowest beds. Excursion to Lyme Regis, May 31st 1914. Some of the more marly beds contain pebble like concretions composed of limestone similar to the white limestone. These stand out on the weathered surface of the rock in small lumps and impart to it a comglomerate appearance. [Caption used as for above].
Page 105 P804415 The White Lias is a white or cream coloured limestone hard and smooth grained in the lowest beds. Excursion to Lyme Regis, May 31st 1914. Some of the more marly beds contain pebble like concretions composed of limestone similar to the white limestone. These stand out on the weathered surface of the rock in small lumps and impart to it a comglomerate appearance. [Caption used as for above].
Page 107 P804416 Fault in White Lias, Pinhay Bay. Excursion to Lyme Regis, May 31st 1914.
Page 107 P804417 Sea cave worn out by the sea in a disturbed portion of the White Lias. Excursion to Lyme Regis, May 31st 1914.
Page 107 P804418 [Coastal erosion]. Excursion to Lyme Regis, May 31st 1914. Owing to the combined action of frost and springs on the one hand and the waves on the other a great amount of waste is going on on this coast the sea lifting blocks out along planes of jointing when the waves dash them about and grind them up.
Page 107 P804419 [Coastal erosion]. Excursion to Lyme Regis, May 31st 1914. Owing to the combined action of frost and springs on the one hand and the waves on the other a great amount of waste is going on on this coast the sea lifting blocks out along planes of jointing when the waves dash them about and grind them up.
Page 109 P804420 Pinhay Bay. Excursion to Lyme Regis, May 31st 1914. Owing to the Easterly dip of the Lias beds it is quite easy to trace the upwards succession of these beds. At Pinhay Bay we start eastward along the shore when we see higher and higher beds of the Blue Lias series as we pass over them in succession. [photo is likely missing on this page].
Page 109 P804421 [Limestone ledges]. Excursion to Lyme Regis, May 31st 1914. The beds of limestone or ledges cropping out on the sea shore. These form natural breakwaters but unfortunately the Lyme people allow a cement company to break them up and use them for export thus endangering the cliffs that protect the town.
Page 109 P804422 [Limestone ledges]. Excursion to Lyme Regis, May 31st 1914. The beds of limestone or ledges cropping out on the sea shore. These form natural breakwaters but unfortunately the Lyme people allow a cement company to break them up and use them for export thus endangering the cliffs that protect the town.
Page 111 P804423 Amaltheus Margaritatus. Lyme Regis. Excursion to Lyme Regis, May 31st 1914.
Page 111 P804424 Asteroceras Brookei. Lyme Regis. Excursion to Lyme Regis, May 31st 1914.
Page 111 P804425 Large ammonites on surface of ledge near Seven Rock Point. This ammonite cemetery contains specimens from 12 to 18 inches in diameter. Excursion to Lyme Regis, May 31st 1914.
Page 111 P804426 Large ammonites on surface of ledge near Seven Rock Point. This Ammonite Cemetery contains specimens from 12 to 18 inches in diameter. Excursion to Lyme Regis, May 31st 1914.
Page 113 P804427 Looking West over Charmouth from a field near the top of Stonebarrow Lane E. of Charmouth. Excursion to Lyme Regis, June 1st 1914.
Page 113 P804428 Looking E.N.E. from near the Lyme Road just East of the Bellows over Charmouth Village. Excursion to Lyme Regis, June 1st 1914.
Page 115 P804429 View of Charmouth Beach from Cockpits. The rocks in the foreground are the Canary Ledges, the first stages in a recent plane of marine denudation. Excursion to Lyme Regis, June 1st 1914.
Page 115 P804430 Undulating strata at about the level of the Lower and Upper Cement Beds capped with much drift and Hill creep. Mouth of the River Char. Excursion to Lyme Regis, June 1st 1914.
Page 117 P804431 The large amphitheatre shaped hollow in Stonebarrow Cliff immediately west of Fairy Dell. Excursion to Lyme Regis, June 1st 1914. Between June 1908 and 1909 a large fall occurred here exposing a fine section of the fault on the right or eastern side of the hollow. Added note: Drift, Foxmould, Sand of the Cowstone horizon, Gault.
Page 117 P804432 The large amphitheatre shaped hollow in Stonebarrow Cliff immediately west of Fairy Dell. Excursion to Lyme Regis, June 1st 1914. Between June 1908 and 1909 a large fall occurred here exposing a fine section of the fault on the right or eastern side of the hollow.
Page 117 P804433 The Western bank of the amphitheatre shaped hollow. Excursion to Lyme Regis, June 1st 1914.
Page 117 P804434 The Seaward Cliff below Fairy Dell in Belemnite Marls. Excursion to Lyme Regis, June 1st 1914. Added note: Belemnite Marls.
Page 119 P804435 Black Ven looking East from the Western end about 3/4 mile from both Charmouth and Lyme. Excursion to Lyme Regis, June 1st 1914.
Page 119 P804436 Black Ven looking East from the Western end about 3/4 mile from both Charmouth and Lyme. Excursion to Lyme Regis, June 1st 1914.
Page 119 P804437 Fairy Dell looking East from its extreme western end. Excursion to Lyme Regis, June 1st 1914.
Page 119 P804438 Fairy Dell looking East from its extreme western end. Excursion to Lyme Regis, June 1st 1914.
Page 121 P804439 Ground Plan and Sections of the Great Landslip at Great and Little Bindon and Dowlands in the Parish of Axmouth on the East Coast of Devon, which took place on the 25th December 1839. Excursion to Lyme Regis, June 1st 1914. [Numbering on photos ignored]. [Many annotations on section not transcribed].
Page 121 P804440 Geological Section of the Chasm, Undercliff and New Raised Beach. From the Eastern Boundary of Great Bindon to the Sea. Excursion to Lyme Regis, June 1st 1914. [Numbering on photos ignored]. [Many annotations on section not transcribed].
Page 121 P804441 Geological View of the Coast from Lyme Regis in the County of Devon to Axmouth Harbour on the East Coast of Devon. Excursion to Lyme Regis, June 1st 1914. [Left hand end of 4] [Numbering on photos ignored]. [Many annotations on section not transcribed].
Page 121 P804442 Geological View of the Coast from Lyme Regis in the County of Devon to Axmouth Harbour on the East Coast of Devon. Excursion to Lyme Regis, June 1st 1914. [Right hand end of 3] [Numbering on photos ignored]. [Many annotations on section not transcribed].
Page 123 P804443 A view of the Landslip from Great Bindon. Excursion to Lyme Regis, June 1st 1914. [Right hand end of 3] [Numbering on photos ignored].
Page 123 P804444 View of the Great Chasm from its Western end at Bindon. Excursion to Lyme Regis, June 1st 1914. [Right hand end of 3] [Numbering on photos ignored].
Page 125 P804445 View of the Landslip at Whitlands, about one mile to the Eastward of the great Chasm at Dowlands which took place on the 3rd of February 1840. Excursion to Lyme Regis, June 1st 1914. Pentire Haven - Contorted Frasnian beds [incorrect title]. [Artist's impression].
Page 125 P804446 Landslip under Southdown between Beer Head and Branscombe, which took place in 1789-90 looking Westward to Sidmouth Torbay and the Start Point. Excursion to Lyme Regis, June 1st 1914. Pentire Haven - Sill in Frasnian beds [incorrect title]. [Artist's impression].
Page 125 P804447 View from the New Beach, looking Westward to Beer Head. Excursion to Lyme Regis, June 1st 1914. [Artist's impression].
Page 125 P804448 View from the Western end of the beach near Culverhole Point, looking Eastward. Excursion to Lyme Regis, June 1st 1914. [Artist's impression].
Page 127 P804449 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 127 P804450 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 127 P804451 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 127 P804452 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 129 P804453 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 129 P804454 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 129 P804455 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 129 P804456 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 131 P804457 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 131 P804458 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 131 P804459 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 131 P804460 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 133 P804461 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 133 P804462 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 133 P804463 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 133 P804464 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 135 P804465 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 135 P804466 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 135 P804467 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 135 P804468 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 137 P804469 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 137 P804470 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 137 P804471 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 137 P804472 The Landslip. Excursion to Lyme Regis, June 2nd 1914.
Page 139 P804473 The Great Cleft is a fissure running parallel to the face of the cliff thus cutting off a thick slide of rock. Excursion to Lyme Regis, June 2nd 1914. The crack first started in 1886 and had gradually widened year by year but rather more rapidly of late than at first. The base is cut in Upper Greensand the cherty nature of which is is [sic] well seen. Next comes the Lower Chalk about 3ft thick and then White Chalk of the zone of Rhynchonella cuvieri 60 feet thick followed by 71 feet of Terebratulina gracilis zone.
Page 139 P804474 The Great Cleft is a fissure running parallel to the face of the cliff thus cutting off a thick slide of rock. Excursion to Lyme Regis, June 2nd 1914. The crack first started in 1886 and had gradually widened year by year but rather more rapidly of late than at first. The base is cut in Upper Greensand the cherty nature of which is is [sic] well seen. Next comes the Lower Chalk about 3ft thick and then White Chalk of the zone of Rhynchonella cuvieri 60 feet thick followed by 71 feet of Terebratulina gracilis zone.
Page 139 P804475 The Great Cleft is a fissure running parallel to the face of the cliff thus cutting off a thick slide of rock. Excursion to Lyme Regis, June 2nd 1914. The crack first started in 1886 and had gradually widened year by year but rather more rapidly of late than at first. The base is cut in Upper Greensand the cherty nature of which is is [sic] well seen. Next comes the Lower Chalk about 3ft thick and then White Chalk of the zone of Rhynchonella cuvieri 60 feet thick followed by 71 feet of Terebratulina gracilis zone.
Page 139 P804476 The Great Cleft is a fissure running parallel to the face of the cliff thus cutting off a thick slide of rock. Excursion to Lyme Regis, June 2nd 1914. The crack first started in 1886 and had gradually widened year by year but rather more rapidly of late than at first. The base is cut in Upper Greensand the cherty nature of which is is [sic] well seen. Next comes the Lower Chalk about 3ft thick and then White Chalk of the zone of Rhynchonella cuvieri 60 feet thick followed by 71 feet of Terebratulina gracilis zone.
Page 141 P804477 The Chapel Rock. Excursion to Lyme Regis, June 2nd 1914. The Chapel Rock is a lofty detached mass of Chalk of the zones of Terebratulina gracilis, Holaster planus, and Micraster cor-testudinarium which has slipped from the main face of Pinhay Cliffs. It is between 120 and 130 ft high.
Page 141 P804478 The Chapel Rock. Excursion to Lyme Regis, June 2nd 1914. The Chapel Rock is a lofty detached mass of Chalk of the zones of Terebratulina gracilis, Holaster planus, and Micraster cor-testudinarium which has slipped from the main face of Pinhay Cliffs. It is between 120 and 130 ft high.
Page 141 P804479 Rhacoceras loscombei. Lyme Regis. Excursion to Lyme Regis, June 2nd 1914.
Page 141 P804480 Rhacoceras loscombei. Lyme Regis. Excursion to Lyme Regis, June 2nd 1914.
Page 143 P804481 Charton Bay. Excursion to Lyme Regis, June 2nd 1914. The higher portions are seen to include the Black Shales and White Lias estimated to be 25 feet thick while the lower portions consist of alternations of hard and soft marls passing gradually into the red and green marls of the Keuper.
Page 143 P804482 Charton Bay. Excursion to Lyme Regis, June 2nd 1914. The higher portions are seen to include the Black Shales and White Lias estimated to be 25 feet thick while the lower portions consist of alternations of hard and soft marls passing gradually into the red and green marls of the Keuper.
Page 143 P804483 Pinhay Bay. This ravine and watercourse coincides with a fault that throws down the Blue Lias limestones some 40 feet on the west. On the east the lowest beds of the Lias are seen resting on the White Lias. Excursion to Lyme Regis, June 2nd 1914.
Page 143 P804484 Humble Point. Excursion to Lyme Regis, June 2nd 1914.
Page 145 P804485 Excursion to Lyme Regis, June 2nd 1914. [Person].
Page 145 P804486 Excursion to Lyme Regis, June 2nd 1914. [People].
Page 145 P804487 At Charton Bay the entire sequence of the Rhaetic Beds can be seen. Excursion to Lyme Regis, June 2nd 1914. The beds are bent into a gentle anticline at the base of which traces of grey marls with reddish tinges may be detected. Above come the grey marls with shale beds, greenish marls and laminated mudstones. Then the Black Shales followed by mammillated Landscape stone and capped by White Lias. [People].
Page 145 P804488 At Charton Bay the entire sequence of the Rhaetic Beds can be seen. Excursion to Lyme Regis, June 2nd 1914. The beds are bent into a gentle anticline at the base of which traces of grey marls with reddish tinges may be detected. Above come the grey marls with shale beds, greenish marls and laminated mudstones. Then the Black Shales followed by mammillated Landscape stone and capped by White Lias. [People].
Page 147 P804489 The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. On the West side of the Valley of the Axe at South Down between Beer and Branscombe a very considerable landslip occurred in March 1790 which for importance and picturesque effect was unrivalled until the later convulsion at Bindon.
Page 147 P804490 The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. Here in the middle of the night a tract of from seven to ten acres ranging along the brow of a steep cliff immediately overhanging the sea suddenly sank down from 200 to 260 feet presenting a striking group of shattered pinnacles and columns of chalk intermingled with the sunken fragments of the fields thus torn awar from their native site.
Page 147 P804491 The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The remains of hedges still traversed these fragments and a stile was seen undisturbed on the summit of one of the subsided columnar masses. The eye looking from above on this wild scene of ruin saw it finely backed by the deep blue of the channel beneath for in this case the landslip in question formed the first term in the commencement of a new and incipient undercliff which fresh falls and the lapse of centuries will be required to bring into the state of that between Lyme and Seaton.
Page 147 P804492 The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The remains of hedges still traversed these fragments and a stile was seen undisturbed on the summit of one of the subsided columnar masses. The eye looking from above on this wild scene of ruin saw it finely backed by the deep blue of the channel beneath for in this case the landslip in question formed the first term in the commencement of a new and incipient undercliff which fresh falls and the lapse of centuries will be required to bring into the state of that between Lyme and Seaton.
Page 149 P804493 The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. It is stated that many previous symptoms had foreshown this catastrophe. A fissure had opened along the line where the disruption afterwards occurred, for months before the subsidence ensued. Another previous sign was given by the stoppage about two years before of a copious stream of very fine water which used to flow out and just below the freestone quarry opened then as now about the middle of the cliff.
Page 149 P804494 The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. It is stated that many previous symptoms had foreshown this catastrophe. A fissure had opened along the line where the disruption afterwards occurred, for months before the subsidence ensued. Another previous sign was given by the stoppage about two years before of a copious stream of very fine water which used to flow out and just below the freestone quarry opened then as now about the middle of the cliff.
Page 149 P804495 The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The strong persuasion of the neighbours connects this with the cause of the subsequent convulsion and the probable opinion is that it had forced a new channel through some of the fissures which were then opening. A fresh stream broke out after the landslip nearer the beach.
Page 149 P804496 The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The strong persuasion of the neighbours connects this with the cause of the subsequent convulsion and the probable opinion is that it had forced a new channel through some of the fissures which were then opening. A fresh stream broke out after the landslip nearer the beach.
Page 151 P804497 The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The subsided mass pressed forward into the sea so as to approach within 100 yards of a submarine crag called the Sherborne Rock which before then was about 400 yards from the coast line. This subsidence was attended by the same phenomenon as at Culverhole and Whitelands namely the elevation of the adjacent submarine rocks for the fishermen related that joints in which they had laid their crab pots beneath the water and over which they had sailed the night before with a depth of 8 or 10 feet they found to their astonishment raised far above the sea level on the next morning with their pots stranded on a reef at a height of 15 ft in the air. As the catastrophe occurred during the night no eye witnessed it but the fishermen who were out (the night being fine) were alarmed by the continual cracking of the cliff.
Page 151 P804498 The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The subsided mass pressed forward into the sea so as to approach within 100 yards of a submarine crag called the Sherborne Rock which before then was about 400 yards from the coast line. This subsidence was attended by the same phenomenon as at Culverhole and Whitelands namely the elevation of the adjacent submarine rocks for the fishermen related that joints in which they had laid their crab pots beneath the water and over which they had sailed the night before with a depth of 8 or 10 feet they found to their astonishment raised far above the sea level on the next morning with their pots stranded on a reef at a height of 15 ft in the air. As the catastrophe occurred during the night no eye witnessed it but the fishermen who were out (the night being fine) were alarmed by the continual cracking of the cliff.
Page 151 P804499 The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The subsided mass pressed forward into the sea so as to approach within 100 yards of a submarine crag called the Sherborne Rock which before then was about 400 yards from the coast line. This subsidence was attended by the same phenomenon as at Culverhole and Whitelands namely the elevation of the adjacent submarine rocks for the fishermen related that joints in which they had laid their crab pots beneath the water and over which they had sailed the night before with a depth of 8 or 10 feet they found to their astonishment raised far above the sea level on the next morning with their pots stranded on a reef at a height of 15 ft in the air. As the catastrophe occurred during the night no eye witnessed it but the fishermen who were out (the night being fine) were alarmed by the continual cracking of the cliff.
Page 151 P804500 The Hooken Cliffs. [Excursion to Lyme Regis, June 2nd 1914]. The subsided mass pressed forward into the sea so as to approach within 100 yards of a submarine crag called the Sherborne Rock which before then was about 400 yards from the coast line. This subsidence was attended by the same phenomenon as at Culverhole and Whitelands namely the elevation of the adjacent submarine rocks for the fishermen related that joints in which they had laid their crab pots beneath the water and over which they had sailed the night before with a depth of 8 or 10 feet they found to their astonishment raised far above the sea level on the next morning with their pots stranded on a reef at a height of 15 ft in the air. As the catastrophe occurred during the night no eye witnessed it but the fishermen who were out (the night being fine) were alarmed by the continual cracking of the cliff.
Page 153 P804501 Microceroceras birchii. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].
Page 153 P804502 Androgynoceras lataecosta. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].
Page 153 P804503 Echioceras raricostatum. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].
Page 153 P804504 Deroceras armatum. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].
Page 155 P804505 Amblycoceras planicosta. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].
Page 155 P804506 Amblycoceras planicosta. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].
Page 155 P804507 Asteroceras oobtusum Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].
Page 155 P804508 [Slab of ammonites]. [Excursion to Lyme Regis, June 2nd 1914]. [No caption].
Page 157 P804509 Oxynoticeras lymensis. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].
Page 157 P804510 Oxynoticeras victoris. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].
Page 157 P804511 Oxynoticeras oxynotum, Lyme Regis. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].
Page 157 P804512 Lytoceras lineatum. Lyme Regis. [Excursion to Lyme Regis, June 2nd 1914].