Editing T W Reader geological photographs, long excursions 1914. Part 1 - index, GA 'Carreck Archive'

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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA001#v=d&z=2&n=5&i=P802509.jp2&y=305&x=437 Page 63]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392521 P804205] || Cataclews. North Cornwall, April 15th 1914. Sections of Minverite at Cataclews Point. The Minverite occurs as Sills interfolded with slates. It is at Cataclews a rather fine grained holocrystalline aggregate of deep brown hornblende, biotite, serpentinous pseudomorphs after olivine, small crystals of Augite and decomposed feldspars with abundant grains and needles of apatite and iron ores. [People].
 
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA001#v=d&z=2&n=5&i=P802509.jp2&y=305&x=437 Page 63]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392521 P804205] || Cataclews. North Cornwall, April 15th 1914. Sections of Minverite at Cataclews Point. The Minverite occurs as Sills interfolded with slates. It is at Cataclews a rather fine grained holocrystalline aggregate of deep brown hornblende, biotite, serpentinous pseudomorphs after olivine, small crystals of Augite and decomposed feldspars with abundant grains and needles of apatite and iron ores. [People].
 
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA001#v=d&z=2&n=5&i=P802509.jp2&y=305&x=437 Page 63]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392522 P804206] || Cataclews. North Cornwall, April 15th 1914. Sections of Minverite at Cataclews Point. The Minverite occurs as Sills interfolded with slates. It is at Cataclews a rather fine grained holocrystalline aggregate of deep brown hornblende, biotite, serpentinous pseudomorphs after olivine, small crystals of Augite and decomposed feldspars with abundant grains and needles of apatite and iron ores. [Person].
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[http://pubs.bgs.ac.uk/publications.html?pubID=GA001#v=d&z=2&n=5&i=P802509.jp2&y=305&x=437 Page 63]
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| GA001 || [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392522 P804206] || Cataclews. North Cornwall, April 15th 1914. Sections of Minverite at Cataclews Point. The Minverite occurs as Sills interfolded with slates. It is at Cataclews a rather fine grained holocrystalline aggregate of deep brown hornblende, biotite, serpentinous pseudomorphs after olivine, small crystals of Augite and decomposed feldspars with abundant grains and needles of apatite and iron ores. [Person].
 
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| [http://pubs.bgs.ac.uk/publications.html?pubID=GA001#v=d&z=2&n=5&i=P802511.jp2&y=305&x=439 Page 65]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392523 P804207] || Marble cliffs, Porthmissen, in Upper Devonian limestone. North Cornwall, April 15th 1914.  
 
| [http://pubs.bgs.ac.uk/publications.html?pubID=GA001#v=d&z=2&n=5&i=P802511.jp2&y=305&x=439 Page 65]|| [http://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=392523 P804207] || Marble cliffs, Porthmissen, in Upper Devonian limestone. North Cornwall, April 15th 1914.  

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