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

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[http://pubs.bgs.ac.uk/publications.html?pubID=GA006 Link to full album]
 
[http://pubs.bgs.ac.uk/publications.html?pubID=GA006 Link to full album]
  
== Nottingham Excursion, May, 1913 ==
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{| class="wikitable"
 
{| 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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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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| GA006 || [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 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802993.jp2&y=305&x=921 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802993.jp2&y=305&x=921 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802995.jp2&y=305&x=923 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802995.jp2&y=305&x=923 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802995.jp2&y=305&x=923 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802995.jp2&y=305&x=923 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802997.jp2&y=305&x=925 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802997.jp2&y=305&x=925 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802997.jp2&y=305&x=925 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802997.jp2&y=305&x=925 Page 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].
+
| GA006 || [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].
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802999.jp2&y=305&x=927 Page 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.
+
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393361 P805045] || Sneinton. Nottingham Excursion, 14th May 1913. Added note: Keuper Conglomerate, Keuper Waterstones.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802999.jp2&y=305&x=927 Page 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].
+
| GA006 || [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].
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802999.jp2&y=305&x=927 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P802999.jp2&y=305&x=927 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803001.jp2&y=305&x=929 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803001.jp2&y=305&x=929 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803001.jp2&y=305&x=929 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803001.jp2&y=305&x=929 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803003.jp2&y=305&x=931 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803003.jp2&y=305&x=931 Page 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.
+
| GA006 || [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.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803003.jp2&y=305&x=931 Page 29]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393371 P805055] || Nottingham Excursion, 14th May 1913. Bunter beds.
+
| GA006 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393371 P805055] || Nottingham Excursion, 14th May 1913. Bunter beds.
 
|-
 
|-
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA006#v=d&z=2&n=5&i=P803003.jp2&y=305&x=931 Page 29]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393372 P805056] || Nottingham Excursion, 14th May 1913. Bunter beds.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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  
+
| GA006 || [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 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  
+
| GA006 || [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 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  
+
| GA006 || [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 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  
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 45]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393397 P805081] || Coverack. Excursion to the Lizard, March 21st 1913. Gabbro pegmatite.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 53]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393415 P805099] || Chynhalls Point. Excursion to the Lizard, March 23rd 1913.  
+
| GA006 || [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 53]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=393416 P805100] || Chynhalls Point. Excursion to the Lizard, March 23rd 1913.  
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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.
+
| GA006 || [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 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 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.

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