Editing T W Reader geological photographs, long excursions 1913 - index, GA 'Carreck Archive'

== T W Reader geological photographs, long excursions 1913 - index, GA 'Carreck Archive' ==

[http://pubs.bgs.ac.uk/publications.html?pubID=GA006 Link to full album]

== Nottingham Excursion, May, 1913 ==

{| class="wikitable"
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802979.jp2&y=305&x=907 Page&nbsp;5]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393321 P805005] || The Vale of Belvoir. Ironstone Quarry Stonepit Houses near Wartnaby. Nottingham Excursion, 10th May 1913. Middle Lias Ironstone.  This ironstone is of the same horizon as the celebrated Cleveland iron ore which belongs to the Marlstone or upper part of the Middle Lias.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802979.jp2&y=305&x=907 Page&nbsp;5]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393322 P805006] || The Vale of Belvoir. Ironstone Quarry Stonepit Houses near Wartnaby. Nottingham Excursion, 10th May 1913. Ironstone overlaid by Boulder Clay. This Ironstone is of the same horizon as the celebrated Cleveland iron ore which belongs to the Marlstone or upper part of the Middle Lias.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802979.jp2&y=305&x=907 Page&nbsp;5]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393323 P805007] || The Vale of Belvoir. Ironstone Quarry Stonepit Houses near Wartnaby. Nottingham Excursion, 10th May 1913. Step-fault in Ironstone with 'Roche Moutonnee' surface. The hollow was originally filled with Upper Lias Clay which has to be removed together with the Boulder Clay before the ironstone can be used.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802979.jp2&y=305&x=907 Page&nbsp;5]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393324 P805008] || The Vale of Belvoir. Ironstone Quarry Stonepit Houses near Wartnaby. Nottingham Excursion, 10th May 1913. Method of working the ironstone. All the clay and top hamper is wheeled across these boards and deposited on the opposite side as the ironstone is removed in the rail trucks, thus causing a flat surface but at a lower level than before.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802981.jp2&y=305&x=909 Page&nbsp;7]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393325 P805009] || The Vale of Belvoir. Stonepit Houses near Wartnaby. Nottingham Excursion, 10th May 1913. Striated surface of ironstone. This is the most southernly ice striated surface in England (Lamplugh).
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802981.jp2&y=305&x=909 Page&nbsp;7]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393326 P805010] || The Vale of Belvoir. Holwell. Nottingham Excursion, 10th May 1913. Face of ironstone.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802981.jp2&y=305&x=909 Page&nbsp;7]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393327 P805011] || The Vale of Belvoir. Holwell. Nottingham Excursion, 10th May 1913. These workings are examples of 'open cast' workings. This brown ironstone is found in a sheet about 14 feet thick generally covered by Boulder Clay which has preserved the scratched and irregular surface caused by moving ice.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802981.jp2&y=305&x=909 Page&nbsp;7]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393328 P805012] || The Vale of Belvoir. Holwell. Nottingham Excursion, 10th May 1913. These workings are examples of 'open cast' workings. This brown ironstone is found in a sheet about 14 feet thick generally covered by Boulder Clay which has preserved the scratched and irregular surface caused by moving ice.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802983.jp2&y=305&x=911 Page&nbsp;9]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393329 P805013] || The Vale of Belvoir. . Nottingham Excursion, 10th May 1913. Marlstone escarpment near Wartnaby. The level ground at the base of this escarpment forms the Vale of Belvoir which is composed of Lower Lias beds and in the distance merges into the plain formed of Keuper marls.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802983.jp2&y=305&x=911 Page&nbsp;9]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393330 P805014] || The Vale of Belvoir. Nottingham Excursion, 10th May 1913. The Vale of Belvoir from edge of escarpment. The level ground at the base of this escarpment forms the Vale of Belvoir which is composed of Lower Lias beds and in the distance merges into the plain formed of Keuper marls. Added note: Boulder Clay hills, position of Hydraulic limestone escarpment,The low escarpment caused by these limestones separates the Lower Lias plain from the Keuper Marl plain.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802983.jp2&y=305&x=911 Page&nbsp;9]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393331 P805015] || The Vale of Belvoir. Holwell. Nottingham Excursion, 10th May 1913. Coombe formed by spring thrown out at junction of Middle and Lower Lias beds.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802983.jp2&y=305&x=911 Page&nbsp;9]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393332 P805016] || The Vale of Belvoir. Holwell. Nottingham Excursion, 10th May 1913. Coombe formed by spring thrown out at junction of Middle and Lower Lias beds.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802985.jp2&y=305&x=913 Page&nbsp;11]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393333 P805017] || The Vale of Belvoir. Barnstone. Nottingham Excursion, 10th May 1913. The Hydraulic Limestone Series of the Lower Lias. The low escarpment caused by these limestones separates the Lower Lias plain from the Keuper Marl plain in the Vale of Belvoir pictures 9 and 10.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802985.jp2&y=305&x=913 Page&nbsp;11]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393334 P805018] || The Vale of Belvoir. Barnstone. Nottingham Excursion, 10th May 1913. The Hydraulic Limestone Series of the Lower Lias. The low escarpment caused by these limestones separates the Lower Lias plain from the Keuper Marl plain in the Vale of Belvoir pictures 9 and 10.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802985.jp2&y=305&x=913 Page&nbsp;11]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393335 P805019] || The Vale of Belvoir. Barnstone. Nottingham Excursion, 10th May 1913. These consist of bluish grey laminated shales with numerous layers of flaggy argillaceous limestone of a lighter tint. It is quarried for the manufacture of cement, paving stones etc. The thickness is about 20 ft and belongs to the zone of Psiloceras planorbis.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802985.jp2&y=305&x=913 Page&nbsp;11]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393336 P805020] || The Vale of Belvoir. Barnstone. Nottingham Excursion, 10th May 1913. These consist of bluish grey laminated shales with numerous layers of flaggy argillaceous limestone of a lighter tint. It is quarried for the manufacture of cement, paving stones etc. The thickness is about 20 ft and belongs to the zone of Psiloceras planorbis.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802987.jp2&y=305&x=915 Page&nbsp;13]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393337 P805021] || The Vale of Belvoir. Nottingham Excursion, 10th May 1913. Gypsum mine at Cropwell Bishop (situated near base of Hydraulic Limestone escarpment). The gypsum deposits are found near the top of the Keuper Marl. It is now won by driving underground galleries along th thicker and richer beds.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802987.jp2&y=305&x=915 Page&nbsp;13]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393338 P805022] || The Vale of Belvoir. Nottingham Excursion, 10th May 1913. Gypsum mine at Cropwell Bishop (situated near base of Hydraulic Limestone escarpment). The gypsum deposits are found near the top of the Keuper Marl. It is now won by driving underground galleries along th thicker and richer beds.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802987.jp2&y=305&x=915 Page&nbsp;13]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393339 P805023] || The Vale of Belvoir. Nottingham Excursion, 10th May 1913. Satin spar or fibrous gypsum, Cropwell Bishop. This gypsum was originally deposited as a chemical precipitate from the evaporating waters of an inland lake. The above silky and fibrous forms have been caused by subsequent alteration such as recystallisation.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802987.jp2&y=305&x=915 Page&nbsp;13]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393340 P805024] || The Vale of Belvoir. Nottingham Excursion, 10th May 1913. Satin spar or fibrous gypsum, Cropwell Bishop. This gypsum was originally deposited as a chemical precipitate from the evaporating waters of an inland lake. The above silky and fibrous forms have been caused by subsequent alteration such as recystallisation.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802989.jp2&y=305&x=917 Page&nbsp;15]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393341 P805025] || The Trent Valley. Hazleford. Nottingham Excursion, 12th May 1913. View of Trent Valley excavated along the strike of the Keuper Marls. The level of the land from which these views were taken is only a few geet above the water level while on the other side it washes the bases of the hills and in places form cliffs.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802989.jp2&y=305&x=917 Page&nbsp;15] || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393342 P805026] || The Trent Valley. Hazleford. Nottingham Excursion, 12th May 1913. 
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802989.jp2&y=305&x=917 Page&nbsp;15]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393343 P805027] || The Trent Valley. Hazleford. Nottingham Excursion, 12th May 1913. The G.A. fleet.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802989.jp2&y=305&x=917 Page&nbsp;15]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393344 P805028] || The Trent Valley. Hazleford. Nottingham Excursion, 12th May 1913. Keuper Cliff at Hazleford.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802991.jp2&y=305&x=919 Page&nbsp;17]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393345 P805029] || Newark. Nottingham Excursion, 12th May 1913. Gypsum bearing Keuper Marls Messrs Cafferata's Pit.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802991.jp2&y=305&x=919 Page&nbsp;17]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393346 P805030] || Newark. Nottingham Excursion, 12th May 1913. Gypsum bearing Keuper Marls Messrs Cafferata's Pit.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802991.jp2&y=305&x=919 Page&nbsp;17]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393347 P805031] || Newark. Nottingham Excursion, 12th May 1913. The gypsum is found in layers from as much as 15 feet to a mere film. It is very irregular, sometimes being in a continuous deposit and at other in disjointed masses called by the quarrymen 'balls'.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802991.jp2&y=305&x=919 Page&nbsp;17]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393348 P805032] || Newark. Nottingham Excursion, 12th May 1913. The gypsum is found in layers from as much as 15 feet to a mere film. It is very irregular, sometimes being in a continuous deposit and at other in disjointed masses called by the quarrymen 'balls'.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802993.jp2&y=305&x=921 Page&nbsp;19]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393349 P805033] || Newark. Nottingham Excursion, 12th May 1913. Gypsum bearing Keuper Marls, Messrs Cafferata's Pit. The pure gypsum is used for making plaster of Paris, being roasted in a kiln and then ground to fine powder. The poorer qualities are used for cement.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802993.jp2&y=305&x=921 Page&nbsp;19]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393350 P805034] || Newark. Nottingham Excursion, 12th May 1913. Gypsum bearing Keuper Marls, Messrs Cafferata's Pit. The pure gypsum is used for making plaster of Paris, being roasted in a kiln and then ground to fine powder. The poorer qualities are used for cement.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802993.jp2&y=305&x=921 Page&nbsp;19]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393351 P805035] || Newark. Nottingham Excursion, 12th May 1913. Veins of fibrous gypsum. This is 'Satin spar' and used for making beads and small ornaments. Added note: Satin spar is a special kind of fibrous gypsum which is remarkably translucent and at present is quarried in only one place viz East Bridgford. Fibrous gypsum is not sufficently translucent.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802993.jp2&y=305&x=921 Page&nbsp;19]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393352 P805036] || Newark. Nottingham Excursion, 12th May 1913. Balls of gypsum. The clearer and veined portions are known as alabaster and used as ornamental building stone.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802995.jp2&y=305&x=923 Page&nbsp;21]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393353 P805037] || Creswell. Quarry over Church Hole Cave. Nottingham Excursion, 13th May 1913. Swallow hole in Magnesian Limestone. The limestone holds a quantity of water in these spaces but it is not of good quality.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802995.jp2&y=305&x=923 Page&nbsp;21]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393354 P805038] || Creswell. Quarry over Church Hole Cave. Nottingham Excursion, 13th May 1913. Face of Magnesian Limestone. Used as a building stone and consisting mainly of dolomite crystals with quartz sand and free calcite.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802995.jp2&y=305&x=923 Page&nbsp;21]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393355 P805039] || Creswell. Nottingham Excursion, 13th May 1913. Creswell Crags. Entrance to Robin Hood's Cave. The Magnesian Limestone is strongly jointed and some of the joints are enlarged into fissures which expand into wide caves the mouths of which are usually 20 feet above the floor of the ravine.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802995.jp2&y=305&x=923 Page&nbsp;21]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393356 P805040] || Creswell. Nottingham Excursion, 13th May 1913. Creswell Gorge. It is by this gorge that a small tributary of the Poulter breaks across a faulted uplift of the Magnesian Limestone. Added note: Derbyshire on left, Nottinghamshire on right.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802997.jp2&y=305&x=925 Page&nbsp;23]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393357 P805041] || Markland Grips. Nottingham Excursion, 13th May 1913. Fallen block of Magnesian Limestone in a ravine cut in the same rock.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802997.jp2&y=305&x=925 Page&nbsp;23]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393358 P805042] || Markland Grips. Nottingham Excursion, 13th May 1913. Thin bedded Magnesian Limestone of a flaggy character containing quartz grains with granules of dolomite.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802997.jp2&y=305&x=925 Page&nbsp;23]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393359 P805043] || Markland Grips. Langwith. Nottingham Excursion, 13th May 1913. Cave in Magnesian Limestone from which a human skull, many worked flints, and a great variety of bones of extinct and living forms were obtained.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802997.jp2&y=305&x=925 Page&nbsp;23]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393360 P805044] || Markland Grips. Langwith. Nottingham Excursion, 13th May 1913. Railway cutting in Magnesian Limestone. [Group photo].
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802999.jp2&y=305&x=927 Page&nbsp;25]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393361 P805045] || Sneinton. Nottingham Excursion, 14th May 1913. Added note: Keuper Conglomerate, Keuper Waterstones.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802999.jp2&y=305&x=927 Page&nbsp;25]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393362 P805046] || Sneinton. Nottingham Excursion, 14th May 1913. Added note: See details below No. 44. [Group photo].
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802999.jp2&y=305&x=927 Page&nbsp;25]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393363 P805047] || Sneinton. Nottingham Excursion, 14th May 1913. For 18 ft below the Keuper Conglomerate is a series of beds with a peculiar bluish tinge classified at present with Bunter but their stratigraphical relationships however are still uncertain. Added note: Keuper Waterstones, Keuper Conglomerate.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802999.jp2&y=305&x=927 Page&nbsp;25]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393364 P805048] || Sneinton. Nottingham Excursion, 14th May 1913. Pebble band in beds just below the Keuper Conglomerate, position marked in general view above. This shows the resemblance of these beds to Bunter.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803001.jp2&y=305&x=929 Page&nbsp;27]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393365 P805049] || Nottingham Brick Co. Carlton Road. Nottingham Excursion, 14th May 1913. Lower Keuper Marls. These marls although of a clayey texture are mainly silicious silts with carbonates of lime and magnesia shaly and ripple marked with pale greenish bands and thin beds of sandstone called skerries.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803001.jp2&y=305&x=929 Page&nbsp;27]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393366 P805050] || Nottingham Brick Co. Carlton Road. Nottingham Excursion, 14th May 1913. Skerry in Keuper Marls. The thin bands of sandstone are locally known as skerries. When several bands are close together and divided by narrow beds of shale as seen at the top of the section it forms a 'skerry belt' causing a plateau surface.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803001.jp2&y=305&x=929 Page&nbsp;27]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393367 P805051] || Nottingham Brick Co. Carlton Road. Nottingham Excursion, 14th May 1913. Face of Keuper Marls. It is chiefly from these marls that the Nottingham bricks are made.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803001.jp2&y=305&x=929 Page&nbsp;27]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393368 P805052] || Nottingham Brick Co. Carlton Road. Nottingham Excursion, 14th May 1913. Fibrous gypsum in the Keuper Marl between the skerries.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803003.jp2&y=305&x=931 Page&nbsp;29]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393369 P805053] || Bulwell - Magnesian Limestone. Nottingham Excursion, 14th May 1913. Quarry at Bulweel in Permian Lower Limestone. Used for building stone and for making lime.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803003.jp2&y=305&x=931 Page&nbsp;29]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393370 P805054] || Hucknall Road. Nottingham Excursion, 14th May 1913. Bunter beds showing an old channel.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803003.jp2&y=305&x=931 Page&nbsp;29]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393371 P805055] || Nottingham Excursion, 14th May 1913. Bunter beds.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803003.jp2&y=305&x=931 Page&nbsp;29]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393372 P805056] || Nottingham Excursion, 14th May 1913. Bunter beds.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803005.jp2&y=305&x=933 Page&nbsp;31]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393373 P805057] || Bulwell - Brick and Pottery Pits. Nottingham Excursion, 14th May 1913. Permian Marl. A bright red shaly clay or 'marl' with interstratified green layers and thin bands of hard dolomitic sandstone also known as 'Middle Marl'. Used for making superior quality bricks and for flower pots.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803005.jp2&y=305&x=933 Page&nbsp;31]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393374 P805058] || Bulwell - Brick and Pottery Pits. Nottingham Excursion, 14th May 1913. Permian Marl. A bright red shaly clay or 'marl' with interstratified green layers and thin bands of hard dolomitic sandstone also known as 'Middle Marl'. Used for making superior quality bricks and for flower pots.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803005.jp2&y=305&x=933 Page&nbsp;31]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393375 P805059] || Hempshill. Nottingham Excursion, 14th May 1913. Lower Mottled Sandstone with false bedding about 30 ft thick. This is the lowest division of the Bunter having few pebbles and of a fine loamy texture it is of a deep ruddy colour and contains marl interbedded with the sand. Used for moulding sand. The upper coarser portions are used as building sand. Added note: Hempshill Railway Quarry near Bulwell.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803005.jp2&y=305&x=933 Page&nbsp;31]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393376 P805060] || Hempshill. Nottingham Excursion, 14th May 1913. Lower Mottled Sandstone with false bedding about 30 ft thick. This is the lowest division of the Bunter having few pebbles and of a fine loamy texture it is of a deep ruddy colour and contains marl interbedded with the sand. Used for moulding sand. The upper coarser portions are used as building sand. Added note: Hempshill Railway Quarry near Bulwell.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803007.jp2&y=305&x=935 Page&nbsp;33]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393377 P805061] || Kimberley. G. N. R.  Goods Yard. Nottingham Excursion, 14th May 1913. Marl Slates resting on Permian breccia.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803007.jp2&y=305&x=935 Page&nbsp;33]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393378 P805062] || Kimberley. G. N. R.  Goods Yard. Nottingham Excursion, 14th May 1913. Junction of Permian and Coal Measures. The breccia at a low angle resting unconformably upon shaly Coal Measures.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803007.jp2&y=305&x=935 Page&nbsp;33]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393379 P805063] || Kimberley. Midland Railway Cutting. Nottingham Excursion, 14th May 1913. Basement beds consisting of breccia made up of fragments of Carboniferous rocks cemented in a sandy calcareous matrix overlaid by thinly bedded flags on impure sandy dolomite with interbedded grey marl or clay. Added note: Breccia.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803007.jp2&y=305&x=935 Page&nbsp;33]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393380 P805064] || Kimberley. Midland Railway Cutting. Nottingham Excursion, 14th May 1913. Basement beds consisting of breccia made up of fragments of Carboniferous rocks cemented in a sandy calcareous matrix overlaid by thinly bedded flags on impure sandy dolomite with interbedded grey marl or clay. Added note: Breccia.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803009.jp2&y=305&x=937 Page&nbsp;35]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393381 P805065] || The Hemlock Stone. Nottingham Excursion, 15th May 1913. The Hemlock or Himlack Stone stands in a grassy depression between the wooded heights of Stapleford and Bramcote and rises to a height of 31 feet.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803009.jp2&y=305&x=937 Page&nbsp;35]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393382 P805066] || The Hemlock Stone. Nottingham Excursion, 15th May 1913. Owing to its superior hardness it has resisted the destroying action of the rain and frost more than the surrounding rock which has been washed gradually away.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803009.jp2&y=305&x=937 Page&nbsp;35]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393383 P805067] || The Hemlock Stone. Nottingham Excursion, 15th May 1913. It is a natural pillar due to selective atmospheric weathering the capping being a hard conglomerate cemented by barium sulphate. The conglomerate belongs to the top of the Bunter and also forms the summits of the two Hills.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803009.jp2&y=305&x=937 Page&nbsp;35]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393384 P805068] || The Hemlock Stone. Nottingham Excursion, 15th May 1913. False bedding on surface of Hemlock Stone, the portion marked in the view above.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803011.jp2&y=305&x=939 Page&nbsp;37]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393385 P805069] || Gypsum showing the transition from the amorphous to the fibrous form. Nottingham Excursion 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803011.jp2&y=305&x=939 Page&nbsp;37]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393386 P805070] || Pseudomorphs after salt in Lower Keuper Marls, Nottingham Brick Co., Carlton Road, Nottingham. Nottingham Excursion 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803011.jp2&y=305&x=939 Page&nbsp;37]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393387 P805071] || Dreikanters - near Nottingham. Quartzites acted upon during Triassic times by wind driving sand. Nottingham Excursion 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803011.jp2&y=305&x=939 Page&nbsp;37]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393388 P805072] || Dreikanters - near Nottingham. Quartzites acted upon during Triassic times by wind driving sand. Nottingham Excursion 
|}
== Excursion to the Lizard, March, 1913 ==
{|Class="wikitable"
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803015.jp2&y=305&x=943 Page&nbsp;41]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393389 P805073] || Coverack. Excursion to the Lizard, March 20th 1913. The point on which the houses are built is serpentine with dykes of dolerite and veins of gabbro piercing it in every direction.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803015.jp2&y=305&x=943 Page&nbsp;41]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393390 P805074] || Coverack. Excursion to the Lizard, March 20th 1913. The two views were taken from the North, the high ground in the foreground being the gabbro boss.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803015.jp2&y=305&x=943 Page&nbsp;41]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393391 P805075] || Dolor Point. Excursion to the Lizard, March 20th 1913. Serpentine pierced by dykes of troctolite and olivine gabbro, these were at a later data cut by olivine dolerites.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803015.jp2&y=305&x=943 Page&nbsp;41]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393392 P805076] || Dolor Point. Excursion to the Lizard, March 20th 1913. Serpentine pierced by dykes of troctolite and olivine gabbro, these were at a later data cut by olivine dolerites.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803017.jp2&y=305&x=945 Page&nbsp;43]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393393 P805077] || Coverack. Excursion to the Lizard, March 20th 1913. Lowland Point. The broad terrace at the foot of the old gabbro cliff is a raised beach.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803017.jp2&y=305&x=945 Page&nbsp;43]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393394 P805078] || Coverack. Excursion to the Lizard, March 20th 1913. Lowland Point. The raised beach from the village.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803017.jp2&y=305&x=945 Page&nbsp;43]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393395 P805079] || North Corner. Excursion to the Lizard, March 20th 1913. Large blocks broken from the intrusive edge of the gabbro.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803017.jp2&y=305&x=945 Page&nbsp;43]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393396 P805080] || North Corner. Excursion to the Lizard, March 20th 1913. Large blocks broken from the intrusive edge of the gabbro.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803019.jp2&y=305&x=947 Page&nbsp;45]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393397 P805081] || Coverack. Excursion to the Lizard, March 21st 1913. Gabbro pegmatite.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803019.jp2&y=305&x=947 Page&nbsp;45]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393398 P805082] || Coverack. Excursion to the Lizard, March 21st 1913. Standing block of serpentine, this being of a harder nature has resisted denudation longer than the surrounding material.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803019.jp2&y=305&x=947 Page&nbsp;45]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393399 P805083] || Coverack. Excursion to the Lizard, March 21st 1913. Sand grains cemented by marine works 'Sabellaria alveolata' to form protective chambers.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803019.jp2&y=305&x=947 Page&nbsp;45]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393400 P805084] || Coverack. Excursion to the Lizard, March 21st 1913. Sand grains cemented by marine works 'Sabellaria alveolata' to form protective chambers.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803021.jp2&y=305&x=949 Page&nbsp;47]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393401 P805085] || Coverack. Excursion to the Lizard, March 21st 1913. Bastite serpentine cut by gabbro dyke.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803021.jp2&y=305&x=949 Page&nbsp;47]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393402 P805086] || Coverack. Excursion to the Lizard, March 21st 1913. Side of a dolerite dyke exposed by the removal of the serpentine around it. Shows polygonal jointing in the dolerite and spheroidal weathering.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803021.jp2&y=305&x=949 Page&nbsp;47]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393403 P805087] || Coverack. Excursion to the Lizard, March 21st 1913. Narrow black dyke (olivine dolerite) cutting through serpentine raised beach with pebbles at top.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803021.jp2&y=305&x=949 Page&nbsp;47]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393404 P805088] || Coverack. Excursion to the Lizard, March 21st 1913. Reticulate network of cracks developed by action of the weather in bastite serpentine.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803023.jp2&y=305&x=951 Page&nbsp;49]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393405 P805089] || Crousa Downs. Excursion to the Lizard, March 21st 1913. Cromlech called the Brothers of Grugwith.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803023.jp2&y=305&x=951 Page&nbsp;49]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393406 P805090] || Crousa Downs. Excursion to the Lizard, March 21st 1913. Cromlech called the Brothers of Grugwith.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803023.jp2&y=305&x=951 Page&nbsp;49]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393407 P805091] || Crousa Downs. Excursion to the Lizard, March 21st 1913. Residual blocks of gabbro strewn over the surface of the Downs. Owing to the rotting of the exposed surface and the washing away of the fine material the harder portions are left.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803023.jp2&y=305&x=951 Page&nbsp;49]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393408 P805092] || Crousa Downs. Excursion to the Lizard, March 21st 1913. Residual blocks of gabbro strewn over the surface of the Downs. Owing to the rotting of the exposed surface and the washing away of the fine material the harder portions are left.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803025.jp2&y=305&x=953 Page&nbsp;51]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393409 P805093] || Crousa Downs. Excursion to the Lizard, March 21st/22nd 1913. Pliocene gravels.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803025.jp2&y=305&x=953 Page&nbsp;51]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393410 P805094] || Crousa Downs. Excursion to the Lizard, March 21st/22nd 1913. Pliocene gravels resting on Pliocene platform cut out of the gabbro.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803025.jp2&y=305&x=953 Page&nbsp;51]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393411 P805095] || Crousa Downs. Excursion to the Lizard, March 21st/22nd 1913. Pliocene gravel.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803025.jp2&y=305&x=953 Page&nbsp;51]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393412 P805096] || Crousa Downs. Excursion to the Lizard, March 21st/22nd 1913. Nigger-heads or greystones, St. Keverne. These are the blocks that stand out when the soft decomposed gabbro around them is washed away. They show spheroidal weathering.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803027.jp2&y=305&x=955 Page&nbsp;53]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393413 P805097] || Chynhalls Point. Excursion to the Lizard, March 23rd 1913. The headland in the distance is gabbro. This point is a mass of serpentine pierced by dykes of gabbro which are themselves cut by epidiorite dykes.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803027.jp2&y=305&x=955 Page&nbsp;53]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393414 P805098] || Chynhalls Point. Excursion to the Lizard, March 23rd 1913. This point is a mass of serpentine pierced by dykes of gabbro which are themselves cut by epidiorite dykes.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803027.jp2&y=305&x=955 Page&nbsp;53]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393415 P805099] || Chynhalls Point. Excursion to the Lizard, March 23rd 1913. 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803027.jp2&y=305&x=955 Page&nbsp;53]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393416 P805100] || Chynhalls Point. Excursion to the Lizard, March 23rd 1913. 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803029.jp2&y=305&x=957 Page&nbsp;55]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393417 P805101] || Chynhalls Point. Excursion to the Lizard, March 23rd 1913. The sea as an eroding agent.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803029.jp2&y=305&x=957 Page&nbsp;55]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393418 P805102] || Chynhalls Point. Excursion to the Lizard, March 23rd 1913. Fissure weathering of serpentine.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803029.jp2&y=305&x=957 Page&nbsp;55]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393419 P805103] || Chynhalls Point. Excursion to the Lizard, March 23rd 1913. Advanced or prismatic weathering of serpentine.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803029.jp2&y=305&x=957 Page&nbsp;55]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393420 P805104] || Chynhalls Point. Excursion to the Lizard, March 23rd 1913. Advanced or prismatic weathering of serpentine.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803031.jp2&y=305&x=959 Page&nbsp;57]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393421 P805105] || Carrick Luz. Excursion to the Lizard, March 23rd 1913. This dyke of gabbro cutting the serpentine has a breadth of over 100 yards and being harder has been left now forming a long promontory running out to sea.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803031.jp2&y=305&x=959 Page&nbsp;57]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393422 P805106] || Carrick Luz. Excursion to the Lizard, March 23rd 1913. Spernic Cove. Added note: Shows foliation of gabbro (augen gabbro) dipping very steeply to the N.E.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803031.jp2&y=305&x=959 Page&nbsp;57]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393423 P805107] || Carrick Luz. Excursion to the Lizard, March 23rd 1913. Augen gabbro, Carrick Luz.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803031.jp2&y=305&x=959 Page&nbsp;57]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393424 P805108] || Carrick Luz. Excursion to the Lizard, March 23rd 1913. Spernic Cove. Cliffs of serpentine containing dykes of flaser gabbro, granite and epidiorite. Added note: The narrow gully or groove above the arrow marks the junction of the gabbro dyke on the left with the serpentine on the right.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803033.jp2&y=305&x=961 Page&nbsp;59]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393425 P805109] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Section of consolidated crush breccia of the Veryan Series. A fine grained quartzose sandstone with calcareous veins quarried for road metal. Roadside near Carn.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803033.jp2&y=305&x=961 Page&nbsp;59]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393426 P805110] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Head capping Devonian beds, S.W. of Nare Point. Added note: Head, raised beach, slaty Devonian beds.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803033.jp2&y=305&x=961 Page&nbsp;59]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393427 P805111] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Veryan quartzite underlaid by spring thown out at the junction. Added note: Spring.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803033.jp2&y=305&x=961 Page&nbsp;59]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393428 P805112] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Veryan quartzite below Penare. Brecciated and veined with quartz. [Group photo].
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803035.jp2&y=305&x=963 Page&nbsp;61]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393429 P805113] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Platform of head overlying raised beach with Devonian beds below. From Men Aver beach.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803035.jp2&y=305&x=963 Page&nbsp;61]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393430 P805114] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Blk dyke, Coverack.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803035.jp2&y=305&x=963 Page&nbsp;61]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393431 P805115] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Devonian slates and conglomerates, Nare Point.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803035.jp2&y=305&x=963 Page&nbsp;61]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393432 P805116] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Nare Head. Devonian slates with plant remains.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803037.jp2&y=305&x=965 Page&nbsp;63]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393433 P805117] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Dennis Head - Portscatho Series (Ordovician).
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803037.jp2&y=305&x=965 Page&nbsp;63]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393434 P805118] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Gillan Harbour with entrance to Helford River beyond. Devonian series on the South side of Gillan Harbour, and Ordovician rocks (Portscatho series) occupy the Northern area.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803037.jp2&y=305&x=965 Page&nbsp;63]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393435 P805119] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Penare. Veryan beds in the foreground and Devonian conglomerate forms the headland.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803037.jp2&y=305&x=965 Page&nbsp;63]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393436 P805120] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Gillan Harbour. Portscatho series (Ordovician on the left, Devonian beds on the right).
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803039.jp2&y=305&x=967 Page&nbsp;65]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393437 P805121] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Devonian beds, Gillan Harbour.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803039.jp2&y=305&x=967 Page&nbsp;65]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393438 P805122] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Devonian slates, S.W. of Nare Point.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803039.jp2&y=305&x=967 Page&nbsp;65]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393439 P805123] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Spring at Tregithy [Tregithey] thrown out at junction of hornblende schist and Veryan beds.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803039.jp2&y=305&x=967 Page&nbsp;65] || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393440 P805124] || Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803041.jp2&y=305&x=969 Page&nbsp;67]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393441 P805125] || Kennack. Excursion to the Lizard, March 25th 1913. East side of Kennack Sands. Bastite serpentine with thin white steatite veins. A large black syke or inclined sill of epidiorite runs through the serpentine from the points marked.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803041.jp2&y=305&x=969 Page&nbsp;67]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393442 P805126] || Kennack. Excursion to the Lizard, March 25th 1913. Cliff of streaky Kennack gneiss, showing a pale acid portion including and veining a dark basic material.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803041.jp2&y=305&x=969 Page&nbsp;67]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393443 P805127] || Kennack. Excursion to the Lizard, March 25th 1913. Bastite serpentine with veins of steatite. Note the shining little crystals of bastite.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803041.jp2&y=305&x=969 Page&nbsp;67]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393444 P805128] || Kennack. Excursion to the Lizard, March 25th 1913. Bastite serpentine with veins of steatite. Note the shining little crystals of bastite.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803043.jp2&y=305&x=971 Page&nbsp;69]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393445 P805129] || Kennack. Excursion to the Lizard, March 25th 1913. Kennack Sands. Enys Head in background. Beyond that on skyline Ruan Minor village and Grade Church. In middle of bay, the Caerverrack rocks which are serpentine.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803043.jp2&y=305&x=971 Page&nbsp;69]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393446 P805130] || Kennack. Excursion to the Lizard, March 25th 1913. Kennack Sands from West. In foreground the banded Kennack gneisses. In distance the point of Carrick Luz which is the gabbro dyke.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803043.jp2&y=305&x=971 Page&nbsp;69]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393447 P805131] || Kennack. Excursion to the Lizard, March 25th 1913. Kennack gneiss.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803043.jp2&y=305&x=971 Page&nbsp;69]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393448 P805132] || Kennack. Excursion to the Lizard, March 25th 1913. Dyke in serpentine on beach, Kennack.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803045.jp2&y=305&x=973 Page&nbsp;71] || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393449 P805133] || Kennack. Excursion to the Lizard, March 25th 1913. Red granite boss of the banded Kennack gneisses at West corner of Kennack.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803045.jp2&y=305&x=973 Page&nbsp;71]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393450 P805134] || Kennack. Excursion to the Lizard, March 25th 1913. Steatite serpentine.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803045.jp2&y=305&x=973 Page&nbsp;71]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393451 P805135] || Kennack. Excursion to the Lizard, March 25th 1913. Cliff of banded gneiss. West side of Kennack Bay.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803045.jp2&y=305&x=973 Page&nbsp;71] || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393452 P805136] || Kennack. Excursion to the Lizard, March 25th 1913. Bastite serpentine cut by gabbro and both cut by epidiorite. West side of Kennack Bay.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803047.jp2&y=305&x=975 Page&nbsp;73]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393453 P805137] || Cadgwith. Excursion to the Lizard, March 25th 1913. The tunnel is a line of fault, the softer material having been eaten out by the sea forming a cave. The roof having collapsed an amphitheatre has been formed now called the Devils [Devil's] Frying Pan. Added note: The rock on the right is hornblende schist, that on the left is mostly Kennack gneiss.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803047.jp2&y=305&x=975 Page&nbsp;73]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393454 P805138] || Cadgwith. Excursion to the Lizard, March 25th 1913. The tunnel is a line of fault, the softer material having been eaten out by the sea forming a cave. The roof having collapsed an amphitheatre has been formed now called the Devils [Devil's] Frying Pan. Added note: The rock on the right is hornblende schist, that on the left is mostly Kennack gneiss.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803047.jp2&y=305&x=975 Page&nbsp;73]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393455 P805139] || Cadgwith. Excursion to the Lizard, March 25th 1913. Hornblende schist, Cadgwith.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803047.jp2&y=305&x=975 Page&nbsp;73]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393456 P805140] || Excursion to the Lizard, March 25th 1913. Spernic Cove. Shows junction of gabbro dyke on the left with serpentine on the right.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803049.jp2&y=305&x=977 Page&nbsp;75]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393457 P805141] || Lizard Head. Excursion to the Lizard, March 26th 1913. Man of War Rocks. These islands are formed of Man of War gneiss.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803049.jp2&y=305&x=977 Page&nbsp;75]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393458 P805142] || Lizard Head. Excursion to the Lizard, March 26th 1913. Man of War Rocks. These islands are formed of Man of War gneiss.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803049.jp2&y=305&x=977 Page&nbsp;75]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393459 P805143] || Lizard Head. Excursion to the Lizard, March 26th 1913. Pebble of serpentine and steatite.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803049.jp2&y=305&x=977 Page&nbsp;75]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393460 P805144] || Lizard Head. Excursion to the Lizard, March 26th 1913. Gabbro schist.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803051.jp2&y=305&x=979 Page&nbsp;77]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393461 P805145] || Polpeor. Excursion to the Lizard, March 26th 1913. Tremolite serpentine but mostly the pinkish mica schist.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803051.jp2&y=305&x=979 Page&nbsp;77]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393462 P805146] || Polpeor. Excursion to the Lizard, March 26th 1913. Sheared black dyke. Added note: 1: Crumpled mica schist, 2: Large bolster shaped mass or pulled out basalt dyke.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803051.jp2&y=305&x=979 Page&nbsp;77]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393463 P805147] || Polpeor. Excursion to the Lizard, March 26th 1913. Contorted hornblende schist.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803051.jp2&y=305&x=979 Page&nbsp;77]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393464 P805148] || Polpeor. Excursion to the Lizard, March 26th 1913. Cave caused by erosion of fault.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803053.jp2&y=305&x=981 Page&nbsp;79]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393465 P805149] || Kynance. Excursion to the Lizard, March 26th 1913. Tremolite serpentine in foreground and in Lion Rock.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803053.jp2&y=305&x=981 Page&nbsp;79]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393466 P805150] || Kynance. Excursion to the Lizard, March 26th 1913. The Lion Rock. Added note: Showing the fault between the Lion Rock and Yellow Carn headland eaten out by the sea.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803053.jp2&y=305&x=981 Page&nbsp;79]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393467 P805151] || Kynance. Excursion to the Lizard, March 26th 1913. Steeple Rock - a serpentine pillar left by erosion of gneiss and granite each side.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803053.jp2&y=305&x=981 Page&nbsp;79]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393468 P805152] || Kynance. Excursion to the Lizard, March 26th 1913. Tremolite serpentine. At top of cliff a granite gneiss intrusion into the tremolite serpentine. Added note: Granite gneiss, Tremolite serpentine.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803055.jp2&y=305&x=983 Page&nbsp;81]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393469 P805153] || Kynance. Excursion to the Lizard, March 26th 1913. Pebble of serpentine with steatite breccia.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803055.jp2&y=305&x=983 Page&nbsp;81]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393470 P805154] || Kynance. Excursion to the Lizard, March 26th 1913. 
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803055.jp2&y=305&x=983 Page&nbsp;81]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393471 P805155] || Kynance. Excursion to the Lizard, March 26th 1913. Stream Kynance. Note the rugged walls of the serpentine valley.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803055.jp2&y=305&x=983 Page&nbsp;81]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393472 P805156] || Kynance. Excursion to the Lizard, March 26th 1913. Druids Stone in British Village above Kynance.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803057.jp2&y=305&x=985 Page&nbsp;83]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393473 P805157] || Gunwalloe. Excursion to the Lizard, March 27th 1913. Folds in the Baulk Head Devonian Beds, consisting of alterations of sandstones and slates.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803057.jp2&y=305&x=985 Page&nbsp;83]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393474 P805158] || Gunwalloe. Excursion to the Lizard, March 27th 1913. Folds in the Baulk Head Devonian Beds, consisting of alterations of sandstones and slates.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803057.jp2&y=305&x=985 Page&nbsp;83]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393475 P805159] || Gunwalloe. Excursion to the Lizard, March 27th 1913. Folds in sandstone of the Baulk Head Devonian Series. Gunwalloe cliff at Jangye-ryn.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803057.jp2&y=305&x=985 Page&nbsp;83]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393476 P805160] || Gunwalloe. Excursion to the Lizard, March 27th 1913. Folds in sandstone of the Baulk Head Devonian Series. Gunwalloe cliff at Jangye-ryn.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803059.jp2&y=305&x=987 Page&nbsp;85]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393477 P805161] || Gunwalloe to Porthleven. Excursion to the Lizard, March 27th 1913. Helston.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803059.jp2&y=305&x=987 Page&nbsp;85]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393478 P805162] || Gunwalloe to Porthleven. Excursion to the Lizard, March 27th 1913. Coast section of Falmouth Beds from Baulk Head to Looe Bar. Added note: Raised beach platform at base of cliff with cemented gravels resting on rock ledge. Porthleven in distance.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803059.jp2&y=305&x=987 Page&nbsp;85]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393479 P805163] || Gunwalloe to Porthleven. Excursion to the Lizard, March 27th 1913. Manaccan Series, Lower Devonian, Baulk Head.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803059.jp2&y=305&x=987 Page&nbsp;85]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393480 P805164] || Gunwalloe to Porthleven. Excursion to the Lizard, March 27th 1913. Manaccan Series, Lower Devonian, Baulk Head. This photograph shows the cleavage planes transverse to the bedding.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803061.jp2&y=305&x=989 Page&nbsp;87]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393481 P805165] || Looe Bar. Excursion to the Lizard, March 27th 1913. Shingle beach formed chiefly of chalk flints with a few chert pebbles.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803061.jp2&y=305&x=989 Page&nbsp;87]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393482 P805166] || Excursion to the Lizard, March 27th 1913. Looe Bar.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803061.jp2&y=305&x=989 Page&nbsp;87]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393483 P805167] || Excursion to the Lizard, March 27th 1913. Looe Bar looking South.
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803061.jp2&y=305&x=989 Page&nbsp;87]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393484 P805168] || Looe Bar. Excursion to the Lizard, March 27th 1913. The Bar in the distance fronting Looe Pool has converted an original tidal estuary into a freshwater lake. .
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803063.jp2&y=305&x=991 Page&nbsp;89]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393485 P805169] || Porthleven. Excursion to the Lizard, March 27th 1913. The Giant's Rock on beach formed of microcline gneiss, a glacial erratic of 50 tons in weight stranded by ice on the Pleistocene shore.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803063.jp2&y=305&x=991 Page&nbsp;89]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393486 P805170] || Porthleven. Excursion to the Lizard, March 27th 1913. Contorted Mylor banded beds. Note the quartz veins which are crumpled and brecciated.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803063.jp2&y=305&x=991 Page&nbsp;89]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393487 P805171] || Porthleven. Excursion to the Lizard, March 27th 1913. Looe Pool from the Bar. The Falmouth Series occupy all but the most distant parts of the picture.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803063.jp2&y=305&x=991 Page&nbsp;89]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393488 P805172] || Porthleven. Excursion to the Lizard, March 27th 1913. Looe Pool from the Bar. Falmouth Series.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803065.jp2&y=305&x=993 Page&nbsp;91]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393489 P805173] || Kynance to Mullion. Excursion to the Lizard, March 28th 1913. Predannock Head from the South. The cove is Ugo Dour [Ogo-dour] Cove where the serpentine on the right joins the hornblende schist on the left.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803065.jp2&y=305&x=993 Page&nbsp;91]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393490 P805174] || Kynance to Mullion. Excursion to the Lizard, March 28th 1913. In centre of view the celebrated Porstone Point where Messrs Teall and [missing] described the junction of the serpentine and hornblende schist.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803065.jp2&y=305&x=993 Page&nbsp;91]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393491 P805175] || Kynance to Mullion. Excursion to the Lizard, March 28th 1913. The Horse - a mass of tremolite serpentine projecting from the cliff.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803065.jp2&y=305&x=993 Page&nbsp;91]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393492 P805176] || Kynance to Mullion. Excursion to the Lizard, March 28th 1913. At Kynance looking S.E. from the Rill Point. Lion Rock in the distance. Landslip in face of cliff.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803067.jp2&y=305&x=995 Page&nbsp;93]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393493 P805177] || Lizard to Mullion. Excursion to the Lizard, March 28th 1913. Foliated banded hornblende schist in cliffs north of Porstone Point.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803067.jp2&y=305&x=995 Page&nbsp;93]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393494 P805178] || Lizard to Mullion. Excursion to the Lizard, March 28th 1913. Landslip in face of cliffs north of Soap Rock (tremolite serpentine).
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803067.jp2&y=305&x=995 Page&nbsp;93]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393495 P805179] || Lizard to Mullion. Excursion to the Lizard, March 28th 1913. [Landslip in face of cliffs north of Soap Rock (tremolite serpentine).].
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803067.jp2&y=305&x=995 Page&nbsp;93]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393496 P805180] || Lizard to Mullion. Excursion to the Lizard, March 28th 1913. Faulted pebble of hornblende schist.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803069.jp2&y=305&x=997 Page&nbsp;95]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393497 P805181] || Mullion. Excursion to the Lizard, March 28th 1913. Mullion Island consists of pillow lava (spilite) with subordinate beds [of] radiolarian chert and black shales of the Veryan Series.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803069.jp2&y=305&x=997 Page&nbsp;95]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393498 P805182] || Mullion. Excursion to the Lizard, March 28th 1913. Mullion Island consists of pillow lava (spilite) with subordinate beds [of] radiolarian chert and black shales of the Veryan Series.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803069.jp2&y=305&x=997 Page&nbsp;95]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393499 P805183] || Mullion. Excursion to the Lizard, March 28th 1913. An infold of hornblende schist in serpentine, Mullion Cove.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803069.jp2&y=305&x=997 Page&nbsp;95]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393500 P805184] || Mullion. Excursion to the Lizard, March 28th 1913. Hornblende schist.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803071.jp2&y=305&x=999 Page&nbsp;97]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393501 P805185] || Mullion. Excursion to the Lizard, March 28th 1913. Note the raised beach platform at height of 10 feet on Mullion Island.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803071.jp2&y=305&x=999 Page&nbsp;97]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393502 P805186] || Mullion. Excursion to the Lizard, March 28th 1913. Mullion Cove.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803071.jp2&y=305&x=999 Page&nbsp;97]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393503 P805187] || Mullion. Excursion to the Lizard, March 28th 1913. Compact flinty looking serpentine forming the rocky inlet of Henscath.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803071.jp2&y=305&x=999 Page&nbsp;97]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393504 P805188] || Mullion. Excursion to the Lizard, March 28th 1913. The Bumble Rock and cliff of hornblende schist. West of Lizard lighthouses.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803073.jp2&y=305&x=1001 Page&nbsp;99]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393505 P805189] || Mullion. Excursion to the Lizard, March 28th 1913. Shingle beach, Polurrian Cove. The Veryan Series form the headland.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803073.jp2&y=305&x=1001 Page&nbsp;99]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393506 P805190] || Mullion. Excursion to the Lizard, March 28th 1913. Poldhu Marconi Signal Station. On the Veryan slates.
|-
| GA0[http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803073.jp2&y=305&x=1001 Page&nbsp;99]06 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393507 P805191] || Mullion. Excursion to the Lizard, March 28th 1913. Mullion Cove Hotel on hornblende schist. Henscath an islet of fine tremolite serpentine. Behind these Marconi Signal Station.
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803073.jp2&y=305&x=1001 Page&nbsp;99]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393508 P805192] || Mullion. Excursion to the Lizard, March 28th 1913. North point of Polurrian Cove. Veryan Beds.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393509 P805193] || Blue Anchor to Watchet. Minehead Excursion, June 21st 1913. View of Blue Anchor Point showing the anticlinal arrangement of the Keuper Marl.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393510 P805194] || Blue Anchor to Watchet. Minehead Excursion, June 21st 1913. Detailed view of a portion of the cliff depicted in No. 1 showing veins of gypsum.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393511 P805195] || Blue Anchor to Watchet. Minehead Excursion, June 21st 1913. Marine undercutting of Keuper and Rhaetic beds.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393512 P805196] || Blue Anchor to Watchet. Minehead Excursion, June 21st 1913. Rhaetic and Keuper faulted against Keuper.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393513 P805197] || Blue Anchor to Watchet. Minehead Excursion, June 21st 1913. View of fault plane - the face is Keuper Marl.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393514 P805198] || Blue Anchor to Watchet. Minehead Excursion, June 21st 1913. Slipped mass of rock between Blue Anchor and Watchet.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393515 P805199] || Blue Anchor to Watchet. Minehead Excursion, June 21st 1913. Warren Farm section (Upper Keuper). See 2 J. G. Soc. Vol. LXVII Pl. IV.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393516 P805200] || Blue Anchor to Watchet. Minehead Excursion, June 21st 1913. Slipped mass of rock between Blue Anchor and Watchet.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393517 P805201] || St Audries Bay. Minehead Excursion, June 21st 1913. 
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393518 P805202] || St Audries Bay. Minehead Excursion, June 21st 1913. Detailed view of a portion of the cliff at St Audries Bay showing black shales resting on Keuper Grey Marls. Added note: Lower Lias.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393519 P805203] || St Audries Bay. Minehead Excursion, June 21st 1913. Detailed view of a portion of the cliff at St Audries Bay showing black shales resting on Keuper Grey Marls.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393520 P805204] || St Audries Bay. Minehead Excursion, June 21st 1913. Keuper Marls.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393521 P805205] || St Audries Bay. Minehead Excursion, June 21st 1913. Lias beds tilted by landslip. An example of the way horizontal beds are brought within reach of marine erosion.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393522 P805206] || St Audries Bay. Minehead Excursion, June 21st 1913. Black shales overlying the Keuper Grey Marls.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393523 P805207] || St Audries Bay. Minehead Excursion, June 21st 1913. Lias limestone from the above beds when subjected to marine influence besides being rolled by the waves are eaten into by Polydora.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393524 P805208] || Lilstock Bay. Minehead Excursion, June 23rd 1913. 
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393525 P805209] || Lilstock Bay. Minehead Excursion, June 23rd 1913. Section of Lias and Rhaetic Beds. Added note: Lower Lias, Rhaetic.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393526 P805210] || Lilstock Bay. Minehead Excursion, June 23rd 1913. Detailed view of upper part of previous section. Added note: Lower Lias, Watchet Beds, Langport Beds, Cotham Beds, Lilstock Beds or Pteria contorta beds.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393527 P805211] || The Quantocks. Minehead Excursion, June 23rd 1913. Combe looking towards Holford.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393528 P805212] || The Quantocks. Minehead Excursion, June 23rd 1913. Devonian beds. Quarry at entrance to Combe.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393529 P805213] || The Quantocks. Minehead Excursion, June 23rd 1913. Wayside cross at Crowcombe.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393530 P805214] || Woodland Quarry Holford. Minehead Excursion, June 23rd 1913. Hangman's Grits, Devonian.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393531 P805215] || Woodland Quarry Holford. Minehead Excursion, June 23rd 1913. Mesopotamia - between the rivers, Holford.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393532 P805216] || Woodland Quarry Holford. Minehead Excursion, June 23rd 1913. Mesopotamia - between the rivers, Holford.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393533 P805217] || Section in the Trias, Woolston Quarry near Williton. Minehead Excursion, June 24rd 1913. The upper part of the section showing the upper sandstones and upper part of the conglomerate. Added note: Irregularly jointed rubbly red sandstone, Massive even bedded red sandstone, Dark between conglomerate splitting into impersistent even beds, Massive conglomerate with numerous pebbles of Carboniferous limestone which give the rock a grey tint, Upper sandstones Lower Keuper or Upper Bunter, Bunter Conglomerate.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393534 P805218] || Section in the Trias, Woolston Quarry near Williton. Minehead Excursion, June 24rd 1913. North face showing the complete series. Refs. Geol. Quantock Hills, p. 50, Mem. Geol. Surv. 1908, Geol. Mag. 1909 p160-5. Added note: Irregularly jointed rubbly red sandstone, Massive even bedded red sandstone, Dark between conglomerate splitting into impersistent even beds, Massive conglomerate with numerous pebbles of Carboniferous limestone which give the rock a grey tint, Upper sandstones Lower Keuper or Upper Bunter, Bunter Conglomerate.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393535 P805219] || Section in the Trias, Woolston Quarry near Williton. Minehead Excursion, June 24rd 1913. The lower part of the section showing the massive conglomerate.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393536 P805220] || Section in the Trias, Woolston Quarry near Williton. Minehead Excursion, June 24rd 1913. The lower part of the section showing the massive conglomerate with abundant pebbles of Carboniferous limestone many of which are fossiliferous.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393537 P805221] || Section in the Trias, Woolston Quarry near Williton. Minehead Excursion, June 24rd 1913. Section at the West end of the quarry showing nearly the full thickness of the conglomerate. Added note: Conglomerate, Sandstone.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393538 P805222] || Section in the Trias, Woolston Quarry near Williton. Minehead Excursion, June 24rd 1913. View looking East from the West end of the quarry.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393539 P805223] || Section in the Trias, Woolston Quarry near Williton. Minehead Excursion, June 24rd 1913. Bunter Conglomerate.
|-
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393540 P805224] || Section in the Trias, Woolston Quarry near Williton. Minehead Excursion, June 24rd 1913. Joints in the Bunter Conglomerate.
|}

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