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| GA006 || [https://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. _. | | GA006 || [https://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. _. |
Revision as of 12:56, 24 May 2020
Editing T W Reader geological photographs, long excursions 1913 - index, GA 'Carreck Archive'
Link from P numbers currently disabled
GA006 | 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. _. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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). |
GA006 | P805010 | The Vale of Belvoir. Holwell. Nottingham Excursion, 10th May 1913. Face of ironstone. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | P805026 | The Trent Valley. Hazleford. Nottingham Excursion, 12th May 1913. |
GA006 | P805027 | The Trent Valley. Hazleford. Nottingham Excursion, 12th May 1913. The G.A. fleet. |
GA006 | P805028 | The Trent Valley. Hazleford. Nottingham Excursion, 12th May 1913. Keuper Cliff at Hazleford. |
GA006 | P805029 | Newark. Nottingham Excursion, 12th May 1913. Gypsum bearing Keuper Marls Messrs Cafferata's Pit. |
GA006 | P805030 | Newark. Nottingham Excursion, 12th May 1913. Gypsum bearing Keuper Marls Messrs Cafferata's Pit. |
GA006 | 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'. |
GA006 | 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'. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | P805041 | Markland Grips. Nottingham Excursion, 13th May 1913. Fallen block of Magnesian Limestone in a ravine cut in the same rock. |
GA006 | P805042 | Markland Grips. Nottingham Excursion, 13th May 1913. Thin bedded Magnesian Limestone of a flaggy character containing quartz grains with granules of dolomite. |
GA006 | 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. |
GA006 | P805044 | Markland Grips. Langwith. Nottingham Excursion, 13th May 1913. Railway cutting in Magnesian Limestone. [Group photo]. |
GA006 | P805045 | Sneinton. Nottingham Excursion, 14th May 1913. Added note: Keuper Conglomerate, Keuper Waterstones. |
GA006 | P805046 | Sneinton. Nottingham Excursion, 14th May 1913. Added note: See details below No. 44. [Group photo]. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | P805052 | Nottingham Brick Co. Carlton Road. Nottingham Excursion, 14th May 1913. Fibrous gypsum in the Keuper Marl between the skerries. |
GA006 | P805053 | Bulwell - Magnesian Limestone. Nottingham Excursion, 14th May 1913. Quarry at Bulweel in Permian Lower Limestone. Used for building stone and for making lime. |
GA006 | P805054 | Hucknall Road. Nottingham Excursion, 14th May 1913. Bunter beds showing an old channel. |
GA006 | P805055 | Nottingham Excursion, 14th May 1913. Bunter beds. |
GA006 | P805056 | Nottingham Excursion, 14th May 1913. Bunter beds. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | P805061 | Kimberley. G. N. R. Goods Yard. Nottingham Excursion, 14th May 1913. Marl Slates resting on Permian breccia. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | P805068 | The Hemlock Stone. Nottingham Excursion, 15th May 1913. False bedding on surface of Hemlock Stone, the portion marked in the view above. |
GA006 | P805069 | Gypsum showing the transition from the amorphous to the fibrous form. Nottingham Excursion |
GA006 | P805070 | Pseudomorphs after salt in Lower Keuper Marls, Nottingham Brick Co., Carlton Road, Nottingham. Nottingham Excursion |
GA006 | P805071 | Dreikanters - near Nottingham. Quartzites acted upon during Triassic times by wind driving sand. Nottingham Excursion |
GA006 | P805072 | Dreikanters - near Nottingham. Quartzites acted upon during Triassic times by wind driving sand. Nottingham Excursion |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | P805078 | Coverack. Excursion to the Lizard, March 20th 1913. Lowland Point. The raised beach from the village. |
GA006 | P805079 | North Corner. Excursion to the Lizard, March 20th 1913. Large blocks broken from the intrusive edge of the gabbro. |
GA006 | P805080 | North Corner. Excursion to the Lizard, March 20th 1913. Large blocks broken from the intrusive edge of the gabbro. |
GA006 | P805081 | Coverack. Excursion to the Lizard, March 21st 1913. Gabbro pegmatite. |
GA006 | 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. |
GA006 | P805083 | Coverack. Excursion to the Lizard, March 21st 1913. Sand grains cemented by marine works 'Sabellaria alveolata' to form protective chambers. |
GA006 | P805084 | Coverack. Excursion to the Lizard, March 21st 1913. Sand grains cemented by marine works 'Sabellaria alveolata' to form protective chambers. |
GA006 | P805085 | Coverack. Excursion to the Lizard, March 21st 1913. Bastite serpentine cut by gabbro dyke. |
GA006 | 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. |
GA006 | P805087 | Coverack. Excursion to the Lizard, March 21st 1913. Narrow black dyke (olivine dolerite) cutting through serpentine raised beach with pebbles at top. |
GA006 | P805088 | Coverack. Excursion to the Lizard, March 21st 1913. Reticulate network of cracks developed by action of the weather in bastite serpentine. |
GA006 | P805089 | Crousa Downs. Excursion to the Lizard, March 21st 1913. Cromlech called the Brothers of Grugwith. |
GA006 | P805090 | Crousa Downs. Excursion to the Lizard, March 21st 1913. Cromlech called the Brothers of Grugwith. |
GA006 | 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. |
GA006 | 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. |
GA006 | P805093 | Crousa Downs. Excursion to the Lizard, March 21st/22nd 1913. Pliocene gravels. |
GA006 | P805094 | Crousa Downs. Excursion to the Lizard, March 21st/22nd 1913. Pliocene gravels resting on Pliocene platform cut out of the gabbro. |
GA006 | P805095 | Crousa Downs. Excursion to the Lizard, March 21st/22nd 1913. Pliocene gravel. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | P805099 | Chynhalls Point. Excursion to the Lizard, March 23rd 1913. |
GA006 | P805100 | Chynhalls Point. Excursion to the Lizard, March 23rd 1913. |
GA006 | P805101 | Chynhalls Point. Excursion to the Lizard, March 23rd 1913. The sea as an eroding agent. |
GA006 | P805102 | Chynhalls Point. Excursion to the Lizard, March 23rd 1913. Fissure weathering of serpentine. |
GA006 | P805103 | Chynhalls Point. Excursion to the Lizard, March 23rd 1913. Advanced or prismatic weathering of serpentine. |
GA006 | P805104 | Chynhalls Point. Excursion to the Lizard, March 23rd 1913. Advanced or prismatic weathering of serpentine. |
GA006 | 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. |
GA006 | 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. |
GA006 | P805107 | Carrick Luz. Excursion to the Lizard, March 23rd 1913. Augen gabbro, Carrick Luz. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | 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. |
GA006 | P805112 | Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Veryan quartzite below Penare. Brecciated and veined with quartz. [Group photo]. |
GA006 | 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. |
GA006 | P805114 | Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Blk dyke, Coverack. |
GA006 | P805115 | Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Devonian slates and conglomerates, Nare Point. |
GA006 | P805116 | Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Nare Head. Devonian slates with plant remains. |
GA006 | P805117 | Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Dennis Head - Portscatho Series (Ordovician). |
GA006 | 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. |
GA006 | P805119 | Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Penare. Veryan beds in the foreground and Devonian conglomerate forms the headland. |
GA006 | 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). |
GA006 | P805121 | Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Devonian beds, Gillan Harbour. |
GA006 | P805122 | Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] Devonian slates, S.W. of Nare Point. |
GA006 | 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. |
GA006 | P805124 | Nare Head to Manaccan. [Excursion to the Lizard, March 24th 1913.] |
GA006 | 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. |
GA006 | 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. |
GA006 | P805127 | Kennack. Excursion to the Lizard, March 25th 1913. Bastite serpentine with veins of steatite. Note the shining little crystals of bastite. |
GA006 | P805128 | Kennack. Excursion to the Lizard, March 25th 1913. Bastite serpentine with veins of steatite. Note the shining little crystals of bastite. |
GA006 | 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. |
GA006 | 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. |
GA006 | P805131 | Kennack. Excursion to the Lizard, March 25th 1913. Kennack gneiss. |
GA006 | P805132 | Kennack. Excursion to the Lizard, March 25th 1913. Dyke in serpentine on beach, Kennack. |
GA006 | P805133 | Kennack. Excursion to the Lizard, March 25th 1913. Red granite boss of the banded Kennack gneisses at West corner of Kennack. |
GA006 | P805134 | Kennack. Excursion to the Lizard, March 25th 1913. Steatite serpentine. |
GA006 | P805135 | Kennack. Excursion to the Lizard, March 25th 1913. Cliff of banded gneiss. West side of Kennack Bay. |
GA006 | P805136 | Kennack. Excursion to the Lizard, March 25th 1913. Bastite serpentine cut by gabbro and both cut by epidiorite. West side of Kennack Bay. |
GA006 | 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. |
GA006 | 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. |
GA006 | P805139 | Cadgwith. Excursion to the Lizard, March 25th 1913. Hornblende schist, Cadgwith. |
GA006 | P805140 | Excursion to the Lizard, March 25th 1913. Spernic Cove. Shows junction of gabbro dyke on the left with serpentine on the right. |
GA006 | P805141 | Lizard Head. Excursion to the Lizard, March 26th 1913. Man of War Rocks. These islands are formed of Man of War gneiss. |
GA006 | P805142 | Lizard Head. Excursion to the Lizard, March 26th 1913. Man of War Rocks. These islands are formed of Man of War gneiss. |
GA006 | P805143 | Lizard Head. Excursion to the Lizard, March 26th 1913. Pebble of serpentine and steatite. |
GA006 | P805144 | Lizard Head. Excursion to the Lizard, March 26th 1913. Gabbro schist. |
GA006 | P805145 | Polpeor. Excursion to the Lizard, March 26th 1913. Tremolite serpentine but mostly the pinkish mica schist. |
GA006 | 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. |
GA006 | P805147 | Polpeor. Excursion to the Lizard, March 26th 1913. Contorted hornblende schist. |
GA006 | P805148 | Polpeor. Excursion to the Lizard, March 26th 1913. Cave caused by erosion of fault. |
GA006 | P805149 | Kynance. Excursion to the Lizard, March 26th 1913. Tremolite serpentine in foreground and in Lion Rock. |
GA006 | 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. |
GA006 | P805151 | Kynance. Excursion to the Lizard, March 26th 1913. Steeple Rock - a serpentine pillar left by erosion of gneiss and granite each side. |
GA006 | 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. |
GA006 | P805153 | Kynance. Excursion to the Lizard, March 26th 1913. Pebble of serpentine with steatite breccia. |
GA006 | P805154 | Kynance. Excursion to the Lizard, March 26th 1913. |
GA006 | P805155 | Kynance. Excursion to the Lizard, March 26th 1913. Stream Kynance. Note the rugged walls of the serpentine valley. |
GA006 | P805156 | Kynance. Excursion to the Lizard, March 26th 1913. Druids Stone in British Village above Kynance. |
GA006 | P805157 | Gunwalloe. Excursion to the Lizard, March 27th 1913. Folds in the Baulk Head Devonian Beds, consisting of alterations of sandstones and slates. |
GA006 | P805158 | Gunwalloe. Excursion to the Lizard, March 27th 1913. Folds in the Baulk Head Devonian Beds, consisting of alterations of sandstones and slates. |
GA006 | P805159 | Gunwalloe. Excursion to the Lizard, March 27th 1913. Folds in sandstone of the Baulk Head Devonian Series. Gunwalloe cliff at Jangye-ryn. |
GA006 | P805160 | Gunwalloe. Excursion to the Lizard, March 27th 1913. Folds in sandstone of the Baulk Head Devonian Series. Gunwalloe cliff at Jangye-ryn. |
GA006 | P805161 | Gunwalloe to Porthleven. Excursion to the Lizard, March 27th 1913. Helston. |
GA006 | 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. |
GA006 | P805163 | Gunwalloe to Porthleven. Excursion to the Lizard, March 27th 1913. Manaccan Series, Lower Devonian, Baulk Head. |
GA006 | 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. |
GA006 | P805165 | Looe Bar. Excursion to the Lizard, March 27th 1913. Shingle beach formed chiefly of chalk flints with a few chert pebbles. |
GA006 | P805166 | Excursion to the Lizard, March 27th 1913. Looe Bar. |
GA006 | P805167 | Excursion to the Lizard, March 27th 1913. Looe Bar looking South. |
GA006 | 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. . |
GA006 | 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. |
GA006 | P805170 | Porthleven. Excursion to the Lizard, March 27th 1913. Contorted Mylor banded beds. Note the quartz veins which are crumpled and brecciated. |
GA006 | 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. |
GA006 | P805172 | Porthleven. Excursion to the Lizard, March 27th 1913. Looe Pool from the Bar. Falmouth Series. |
GA006 | 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. |
GA006 | 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. |
GA006 | P805175 | Kynance to Mullion. Excursion to the Lizard, March 28th 1913. The Horse - a mass of tremolite serpentine projecting from the cliff. |
GA006 | 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. |
GA006 | P805177 | Lizard to Mullion. Excursion to the Lizard, March 28th 1913. Foliated banded hornblende schist in cliffs north of Porstone Point. |
GA006 | P805178 | Lizard to Mullion. Excursion to the Lizard, March 28th 1913. Landslip in face of cliffs north of Soap Rock (tremolite serpentine). |
GA006 | P805179 | Lizard to Mullion. Excursion to the Lizard, March 28th 1913. [Landslip in face of cliffs north of Soap Rock (tremolite serpentine).]. |
GA006 | P805180 | Lizard to Mullion. Excursion to the Lizard, March 28th 1913. Faulted pebble of hornblende schist. |
GA006 | 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. |
GA006 | 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. |
GA006 | P805183 | Mullion. Excursion to the Lizard, March 28th 1913. An infold of hornblende schist in serpentine, Mullion Cove. |
GA006 | P805184 | Mullion. Excursion to the Lizard, March 28th 1913. Hornblende schist. |
GA006 | P805185 | Mullion. Excursion to the Lizard, March 28th 1913. Note the raised beach platform at height of 10 feet on Mullion Island. |
GA006 | P805186 | Mullion. Excursion to the Lizard, March 28th 1913. Mullion Cove. |
GA006 | P805187 | Mullion. Excursion to the Lizard, March 28th 1913. Compact flinty looking serpentine forming the rocky inlet of Henscath. |
GA006 | P805188 | Mullion. Excursion to the Lizard, March 28th 1913. The Bumble Rock and cliff of hornblende schist. West of Lizard lighthouses. |
GA006 | P805189 | Mullion. Excursion to the Lizard, March 28th 1913. Shingle beach, Polurrian Cove. The Veryan Series form the headland. |
GA006 | P805190 | Mullion. Excursion to the Lizard, March 28th 1913. Poldhu Marconi Signal Station. On the Veryan slates. |
GA006 | 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. |
GA006 | P805192 | Mullion. Excursion to the Lizard, March 28th 1913. North point of Polurrian Cove. Veryan Beds. |
GA006 | P805193 | Blue Anchor to Watchet. Minehead Excursion, June 21st 1913. View of Blue Anchor Point showing the anticlinal arrangement of the Keuper Marl. |
GA006 | 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 | P805195 | Blue Anchor to Watchet. Minehead Excursion, June 21st 1913. Marine undercutting of Keuper and Rhaetic beds. |
GA006 | P805196 | Blue Anchor to Watchet. Minehead Excursion, June 21st 1913. Rhaetic and Keuper faulted against Keuper. |
GA006 | P805197 | Blue Anchor to Watchet. Minehead Excursion, June 21st 1913. View of fault plane - the face is Keuper Marl. |
GA006 | P805198 | Blue Anchor to Watchet. Minehead Excursion, June 21st 1913. Slipped mass of rock between Blue Anchor and Watchet. |
GA006 | 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 | P805200 | Blue Anchor to Watchet. Minehead Excursion, June 21st 1913. Slipped mass of rock between Blue Anchor and Watchet. |
GA006 | P805201 | St Audries Bay. Minehead Excursion, June 21st 1913. |
GA006 | 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 | 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 | P805204 | St Audries Bay. Minehead Excursion, June 21st 1913. Keuper Marls. |
GA006 | 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 | P805206 | St Audries Bay. Minehead Excursion, June 21st 1913. Black shales overlying the Keuper Grey Marls. |
GA006 | 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 | P805208 | Lilstock Bay. Minehead Excursion, June 23rd 1913. |
GA006 | P805209 | Lilstock Bay. Minehead Excursion, June 23rd 1913. Section of Lias and Rhaetic Beds. Added note: Lower Lias, Rhaetic. |
GA006 | 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 | P805211 | The Quantocks. Minehead Excursion, June 23rd 1913. Combe looking towards Holford. |
GA006 | P805212 | The Quantocks. Minehead Excursion, June 23rd 1913. Devonian beds. Quarry at entrance to Combe. |
GA006 | P805213 | The Quantocks. Minehead Excursion, June 23rd 1913. Wayside cross at Crowcombe. |
GA006 | P805214 | Woodland Quarry Holford. Minehead Excursion, June 23rd 1913. Hangman's Grits, Devonian. |
GA006 | P805215 | Woodland Quarry Holford. Minehead Excursion, June 23rd 1913. Mesopotamia - between the rivers, Holford. |
GA006 | P805216 | Woodland Quarry Holford. Minehead Excursion, June 23rd 1913. Mesopotamia - between the rivers, Holford. |
GA006 | 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 | 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 | 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 | 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 | 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 | 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 | P805223 | Section in the Trias, Woolston Quarry near Williton. Minehead Excursion, June 24rd 1913. Bunter Conglomerate. |
GA006 | P805224 | Section in the Trias, Woolston Quarry near Williton. Minehead Excursion, June 24rd 1913. Joints in the Bunter Conglomerate. |