https://earthwise.bgs.ac.uk/index.php?title=Geologists%27_Association_%27green%27_album_1_-_index,_GA_%27Carreck_Archive%27&feed=atom&action=history
Geologists' Association 'green' album 1 - index, GA 'Carreck Archive' - Revision history
2024-03-29T00:33:15Z
Revision history for this page on the wiki
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https://earthwise.bgs.ac.uk/index.php?title=Geologists%27_Association_%27green%27_album_1_-_index,_GA_%27Carreck_Archive%27&diff=46828&oldid=prev
Scotfot: /* Human remains */
2020-07-20T08:34:00Z
<p><span dir="auto"><span class="autocomment">Human remains</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 08:34, 20 July 2020</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wikitable"</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wikitable"</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395065 P806749] || Barrow, with trench. Upware, Cambridgeshire. T.W. Reader. 18.5.14. Human Remains.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803875.jp2&y=305&x=1803 Page&nbsp;89]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395065 P806749] || Barrow, with trench. Upware, Cambridgeshire. T.W. Reader. 18.5.14. Human Remains.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395066 P806750] || Ogams. Near Kilmallock, Ireland. H.A. Haskell. 1921. Human Remains.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803875.jp2&y=305&x=1803 Page&nbsp;89]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395066 P806750] || Ogams. Near Kilmallock, Ireland. H.A. Haskell. 1921. Human Remains.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395067 P806751] || Ogams. Near Kilmallock, Ireland. H.A. Haskell. 1921. Human Remains.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803875.jp2&y=305&x=1803 Page&nbsp;89]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395067 P806751] || Ogams. Near Kilmallock, Ireland. H.A. Haskell. 1921. Human Remains.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395068 P806752] || Cromlach. Near Kilmallock, Ireland. H. Haskell. 192? [1921]. Human Remains.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803875.jp2&y=305&x=1803 Page&nbsp;89]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395068 P806752] || Cromlach. Near Kilmallock, Ireland. H. Haskell. 192? [1921]. Human Remains.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395069 P806753] || Eoliths from drift at Belmont Hill, Lewisham. Drift is in valley of small stream, wh. [which] joined the Quaggy. Material is mostly re-arranged Eocene and a few sub-angular flints. H. Dixon Hewitt. 25.6.05. [Human Remains.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803876.jp2&y=305&x=1804 Page&nbsp;90]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395069 P806753] || Eoliths from drift at Belmont Hill, Lewisham. Drift is in valley of small stream, wh. [which] joined the Quaggy. Material is mostly re-arranged Eocene and a few sub-angular flints. H. Dixon Hewitt. 25.6.05. [Human Remains.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395070 P806754] || Palaeolith. Early S. Acheul ? [sic]. Much abraded. Found at Three Hills (or Warren Hill) Pit, Mildenhall, Suffolk. H. Dixon Hewett [Hewitt]. [Human Remains.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803876.jp2&y=305&x=1804 Page&nbsp;90]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395070 P806754] || Palaeolith. Early S. Acheul ? [sic]. Much abraded. Found at Three Hills (or Warren Hill) Pit, Mildenhall, Suffolk. H. Dixon Hewett [Hewitt]. [Human Remains.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395071 P806755] || Polished pot of volcanic mud and red ochre. [Human Remains.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803876.jp2&y=305&x=1804 Page&nbsp;90]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395071 P806755] || Polished pot of volcanic mud and red ochre. [Human Remains.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395072 P806756] || Implement from Brickearth at Elveden Brickyard, Suffolk. (S. Acheul II period). Found 3'6' below surface in 1915. Now in Ipswich Museum. Edge unworn. H. Dixon Hewett [Hewitt]. [Human Remains.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803876.jp2&y=305&x=1804 Page&nbsp;90]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395072 P806756] || Implement from Brickearth at Elveden Brickyard, Suffolk. (S. Acheul II period). Found 3'6' below surface in 1915. Now in Ipswich Museum. Edge unworn. H. Dixon Hewett [Hewitt]. [Human Remains.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395073 P806757] || Paleolith. S. Acheul Period ? [sic] found at Rarmport? Hill Pit, Icklington, [Icklingham?] Suffolk. Now in Ipswich Museum. H. Dixon Hewett [Hewitt]. 28.9.??. [Human Remains.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803876.jp2&y=305&x=1804 Page&nbsp;90]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395073 P806757] || Paleolith. S. Acheul Period ? [sic] found at Rarmport? Hill Pit, Icklington, [Icklingham?] Suffolk. Now in Ipswich Museum. H. Dixon Hewett [Hewitt]. 28.9.??. [Human Remains.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395074 P806758] || Polishing stone of fine-grained basalt used at the present day by Canarios, at the Troglodite village of Atalaya, Grand Canary in the same manner as in prehistoric times. Photo.d by T.W. Reader. Presented by M.S. Johnston. November 1922. [Human Remains.] Polishing stone of fine-grained basalt used at the present day by Canarios, at the Troglodite village of Atalaya, Grand Canary in the same manner as in prehistoric times. Photo.d by T.W. Reader. Presented by M.S. Johnston. November 1922.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803876.jp2&y=305&x=1804 Page&nbsp;90]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395074 P806758] || Polishing stone of fine-grained basalt used at the present day by Canarios, at the Troglodite village of Atalaya, Grand Canary in the same manner as in prehistoric times. Photo.d by T.W. Reader. Presented by M.S. Johnston. November 1922. [Human Remains.] Polishing stone of fine-grained basalt used at the present day by Canarios, at the Troglodite village of Atalaya, Grand Canary in the same manner as in prehistoric times. Photo.d by T.W. Reader. Presented by M.S. Johnston. November 1922.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[[Category:Geologists' Association Carreck Archive, indexes]]</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[[Category:Geologists' Association Carreck Archive, indexes]]</div></td></tr>
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Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Geologists%27_Association_%27green%27_album_1_-_index,_GA_%27Carreck_Archive%27&diff=46827&oldid=prev
Scotfot: /* Igneous */
2020-07-20T08:32:50Z
<p><span dir="auto"><span class="autocomment">Igneous</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 08:32, 20 July 2020</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l744">Line 744:</td>
<td colspan="2" class="diff-lineno">Line 744:</td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>| [https://pubs.bgs.ac.uk/publications.html?pubID=GA013#v=d&z=2&n=5&i=P803872.jp2&y=305&x=1800 Page&nbsp;86]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395058 P806742] || Columnar Rhyolite (so called 'columnar grit'). Watch Hill near Embleton, Cumberland. W. Hartley. Aug 1920. [Igneous.]</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>| [https://pubs.bgs.ac.uk/publications.html?pubID=GA013#v=d&z=2&n=5&i=P803872.jp2&y=305&x=1800 Page&nbsp;86]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395058 P806742] || Columnar Rhyolite (so called 'columnar grit'). Watch Hill near Embleton, Cumberland. W. Hartley. Aug 1920. [Igneous.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| <del style="font-weight: bold; text-decoration: none;">GA</del>[https://pubs.bgs.ac.uk/publications.html?pubID=GA013#v=d&z=2&n=5&i=P803872.jp2&y=305&x=1800 Page&nbsp;86]<del style="font-weight: bold; text-decoration: none;">013 </del>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395059 P806743] || Fault brecciated surface of Threlkeld Granite. Quarry at Threlkeld, Cumberland. W. Hartley. Aug 1920. [Igneous.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| [https://pubs.bgs.ac.uk/publications.html?pubID=GA013#v=d&z=2&n=5&i=P803872.jp2&y=305&x=1800 Page&nbsp;86] || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395059 P806743] || Fault brecciated surface of Threlkeld Granite. Quarry at Threlkeld, Cumberland. W. Hartley. Aug 1920. [Igneous.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>| [https://pubs.bgs.ac.uk/publications.html?pubID=GA013#v=d&z=2&n=5&i=P803872.jp2&y=305&x=1800 Page&nbsp;86]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395060 P806744] || Edge of columnar rhyolite. Anne Port, Jersey. Miss Yeates. Easter 1922. [Igneous.]</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>| [https://pubs.bgs.ac.uk/publications.html?pubID=GA013#v=d&z=2&n=5&i=P803872.jp2&y=305&x=1800 Page&nbsp;86]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395060 P806744] || Edge of columnar rhyolite. Anne Port, Jersey. Miss Yeates. Easter 1922. [Igneous.]</div></td></tr>
</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Geologists%27_Association_%27green%27_album_1_-_index,_GA_%27Carreck_Archive%27&diff=46826&oldid=prev
Scotfot: /* Igneous */
2020-07-20T08:32:21Z
<p><span dir="auto"><span class="autocomment">Igneous</span></span></p>
<a href="https://earthwise.bgs.ac.uk/index.php?title=Geologists%27_Association_%27green%27_album_1_-_index,_GA_%27Carreck_Archive%27&diff=46826&oldid=46825">Show changes</a>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Geologists%27_Association_%27green%27_album_1_-_index,_GA_%27Carreck_Archive%27&diff=46825&oldid=prev
Scotfot: /* Metamorphic */
2020-07-20T08:28:28Z
<p><span dir="auto"><span class="autocomment">Metamorphic</span></span></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
<col class="diff-marker" />
<col class="diff-content" />
<col class="diff-marker" />
<col class="diff-content" />
<tr class="diff-title" lang="en-GB">
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 08:28, 20 July 2020</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l674">Line 674:</td>
<td colspan="2" class="diff-lineno">Line 674:</td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wikitable"</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wikitable"</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395026 P806710] || Tourmaline schists. Carelaze Pit, St. Austell, Cornwall. Metamorphic.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803863.jp2&y=305&x=1791 Page&nbsp;77]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395026 P806710] || Tourmaline schists. Carelaze Pit, St. Austell, Cornwall. Metamorphic.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395027 P806711] || Spherilitic Adinole. Dinas Head, Pentire. S.H. Reynolds. 15.4.14. Metamorphic.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803863.jp2&y=305&x=1791 Page&nbsp;77]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395027 P806711] || Spherilitic Adinole. Dinas Head, Pentire. S.H. Reynolds. 15.4.14. Metamorphic.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395028 P806712] || Sections in marmolite (serpentine). Pit near Rhoscolyn, Anglesey, N. Wales. Metamorphic.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803863.jp2&y=305&x=1791 Page&nbsp;77]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395028 P806712] || Sections in marmolite (serpentine). Pit near Rhoscolyn, Anglesey, N. Wales. Metamorphic.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395029 P806713] || Sections in marmolite (serpentine). Pit near Rhoscolyn, Anglesey, N. Wales. Metamorphic.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803863.jp2&y=305&x=1791 Page&nbsp;77]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395029 P806713] || Sections in marmolite (serpentine). Pit near Rhoscolyn, Anglesey, N. Wales. Metamorphic.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395030 P806714] || Sections in marmolite (serpentine). Pit near Rhoscolyn, Anglesey, N. Wales. Metamorphic.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803863.jp2&y=305&x=1791 Page&nbsp;77]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395030 P806714] || Sections in marmolite (serpentine). Pit near Rhoscolyn, Anglesey, N. Wales. Metamorphic.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Geologists%27_Association_%27green%27_album_1_-_index,_GA_%27Carreck_Archive%27&diff=46824&oldid=prev
Scotfot: /* Archaean */
2020-07-20T08:27:58Z
<p><span dir="auto"><span class="autocomment">Archaean</span></span></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
<col class="diff-marker" />
<col class="diff-content" />
<col class="diff-marker" />
<col class="diff-content" />
<tr class="diff-title" lang="en-GB">
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 08:27, 20 July 2020</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l648">Line 648:</td>
<td colspan="2" class="diff-lineno">Line 648:</td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wikitable"</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wikitable"</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395015 P806699] || Over-thrust scenery. Quinag from Inchnadampf [Inchnadamph] Hotel. L.J. Wills. July 1914. Archean.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803859.jp2&y=305&x=1787 Page&nbsp;73]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395015 P806699] || Over-thrust scenery. Quinag from Inchnadampf [Inchnadamph] Hotel. L.J. Wills. July 1914. Archean.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395016 P806700] || Over-thrust scenery. Quinag from Loch Glencoul, Scotland. L.J. Wills. July 1914. Archean.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803859.jp2&y=305&x=1787 Page&nbsp;73]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395016 P806700] || Over-thrust scenery. Quinag from Loch Glencoul, Scotland. L.J. Wills. July 1914. Archean.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395017 P806701] || Inverted Lewisian gneiss on streaked out Torridon Sandstone. Lower figure pointing to the junction. Flanks of Ben More, Assynt. L.J. Wills. 7.14. Archean.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803859.jp2&y=305&x=1787 Page&nbsp;73]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395017 P806701] || Inverted Lewisian gneiss on streaked out Torridon Sandstone. Lower figure pointing to the junction. Flanks of Ben More, Assynt. L.J. Wills. 7.14. Archean.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395018 P806702] || Horizontal basal Torridon Sandstone unconformably overlying steeply inclined decomposed Lewisian gneiss. Base of Spidian Coinich (Quinag) nr. Loch Assynt. L. Wills 7.14. Archean.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803859.jp2&y=305&x=1787 Page&nbsp;73]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395018 P806702] || Horizontal basal Torridon Sandstone unconformably overlying steeply inclined decomposed Lewisian gneiss. Base of Spidian Coinich (Quinag) nr. Loch Assynt. L. Wills 7.14. Archean.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395019 P806703] || Dark mylonitized Eastern schists, thrust over white marmolized Cambrian Limestone. South side of the Knockan. Scotland. L.J. Wills. 7.14. Archean.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803859.jp2&y=305&x=1787 Page&nbsp;73]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395019 P806703] || Dark mylonitized Eastern schists, thrust over white marmolized Cambrian Limestone. South side of the Knockan. Scotland. L.J. Wills. 7.14. Archean.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395020 P806704] || The base Moine thrust-plane exposed by the denudation of stream. On right, Eastern schists, white patch in centre, Cambrian Limestone. West side of the Knockan. Scotland. L.J. Wills. 7.14. Archean.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803859.jp2&y=305&x=1787 Page&nbsp;73]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395020 P806704] || The base Moine thrust-plane exposed by the denudation of stream. On right, Eastern schists, white patch in centre, Cambrian Limestone. West side of the Knockan. Scotland. L.J. Wills. 7.14. Archean.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395021 P806705] || Details of Mylonite above the Moine thrust-plane. South side of the Knockan. Scotland. L.J. Wills. 7.14. Archean.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803859.jp2&y=305&x=1787 Page&nbsp;73]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395021 P806705] || Details of Mylonite above the Moine thrust-plane. South side of the Knockan. Scotland. L.J. Wills. 7.14. Archean.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395022 P806706] || Contortions in Pre-Cambrian shale. St. Lawrence Valley, Jersey. W. Hartley. Easter 1921. [Archean.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803860.jp2&y=305&x=1788 Page&nbsp;74]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395022 P806706] || Contortions in Pre-Cambrian shale. St. Lawrence Valley, Jersey. W. Hartley. Easter 1921. [Archean.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395023 P806707] || Vertically inclined Pre-Cambrian shale and greywackes. St. Lawrence Valley, Jersey. W. Hartley. Easter 1921. [Archean.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803860.jp2&y=305&x=1788 Page&nbsp;74]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395023 P806707] || Vertically inclined Pre-Cambrian shale and greywackes. St. Lawrence Valley, Jersey. W. Hartley. Easter 1921. [Archean.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395024 P806708] || 961. [Archean.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803860.jp2&y=305&x=1788 Page&nbsp;74]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395024 P806708] || 961. [Archean.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395025 P806709] || Hutton's unconformity, Lower Carboniferous on Dalradian (pre-Cambrian). [Archean.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803860.jp2&y=305&x=1788 Page&nbsp;74]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395025 P806709] || Hutton's unconformity, Lower Carboniferous on Dalradian (pre-Cambrian). [Archean.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Geologists%27_Association_%27green%27_album_1_-_index,_GA_%27Carreck_Archive%27&diff=46823&oldid=prev
Scotfot: /* Cambrian */
2020-07-20T08:25:37Z
<p><span dir="auto"><span class="autocomment">Cambrian</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 08:25, 20 July 2020</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l642">Line 642:</td>
<td colspan="2" class="diff-lineno">Line 642:</td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>| [https://pubs.bgs.ac.uk/publications.html?pubID=GA013#v=d&z=2&n=5&i=P803855.jp2&y=305&x=1783 Page&nbsp;69]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395013 P806697] || Basement Cambrian conglomerate. Near Tete de [des] Hougues, Bouley Bay, Jersey. W. Hartley. Easter 1921. Cambrian.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>| [https://pubs.bgs.ac.uk/publications.html?pubID=GA013#v=d&z=2&n=5&i=P803855.jp2&y=305&x=1783 Page&nbsp;69]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395013 P806697] || Basement Cambrian conglomerate. Near Tete de [des] Hougues, Bouley Bay, Jersey. W. Hartley. Easter 1921. Cambrian.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| [https://pubs.bgs.ac.uk/publications.html?pubID=GA013#v=d&z=2&n=5&i=<del style="font-weight: bold; text-decoration: none;">P803855</del>.jp2&y=305&x=<del style="font-weight: bold; text-decoration: none;">1783 </del>Page&nbsp;<del style="font-weight: bold; text-decoration: none;">69</del>]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395014 P806698] || Cambrian quartzites dipping at high angle. Boone's Quarry, Tuttle Hill, Nuneaton, Warwicks. H.D. Hewitt. 10.6.35. [Cambrian.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| [https://pubs.bgs.ac.uk/publications.html?pubID=GA013#v=d&z=2&n=5&i=<ins style="font-weight: bold; text-decoration: none;">P803856</ins>.jp2&y=305&x=<ins style="font-weight: bold; text-decoration: none;">1784 </ins>Page&nbsp;<ins style="font-weight: bold; text-decoration: none;">70</ins>]|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395014 P806698] || Cambrian quartzites dipping at high angle. Boone's Quarry, Tuttle Hill, Nuneaton, Warwicks. H.D. Hewitt. 10.6.35. [Cambrian.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Geologists%27_Association_%27green%27_album_1_-_index,_GA_%27Carreck_Archive%27&diff=46822&oldid=prev
Scotfot: /* Cambrian */
2020-07-20T08:24:39Z
<p><span dir="auto"><span class="autocomment">Cambrian</span></span></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 08:24, 20 July 2020</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l638">Line 638:</td>
<td colspan="2" class="diff-lineno">Line 638:</td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wikitable"</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wikitable"</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395012 P806696] || Cambrian rocks sculptured by glacial action. Criccieth, North Wales. T. Kennett Barrington. Cambrian.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803855.jp2&y=305&x=1783 Page&nbsp;69]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395012 P806696] || Cambrian rocks sculptured by glacial action. Criccieth, North Wales. T. Kennett Barrington. Cambrian.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395013 P806697] || Basement Cambrian conglomerate. Near Tete de [des] Hougues, Bouley Bay, Jersey. W. Hartley. Easter 1921. Cambrian.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803855.jp2&y=305&x=1783 Page&nbsp;69]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395013 P806697] || Basement Cambrian conglomerate. Near Tete de [des] Hougues, Bouley Bay, Jersey. W. Hartley. Easter 1921. Cambrian.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395014 P806698] || Cambrian quartzites dipping at high angle. Boone's Quarry, Tuttle Hill, Nuneaton, Warwicks. H.D. Hewitt. 10.6.35. [Cambrian.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803855.jp2&y=305&x=1783 Page&nbsp;69]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395014 P806698] || Cambrian quartzites dipping at high angle. Boone's Quarry, Tuttle Hill, Nuneaton, Warwicks. H.D. Hewitt. 10.6.35. [Cambrian.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td></tr>
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</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Geologists%27_Association_%27green%27_album_1_-_index,_GA_%27Carreck_Archive%27&diff=46821&oldid=prev
Scotfot: /* Silurian */
2020-07-19T23:09:07Z
<p><span dir="auto"><span class="autocomment">Silurian</span></span></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 23:09, 19 July 2020</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l616">Line 616:</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wikitable"</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wikitable"</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395003 P806687] || Silurian rocks scenery. Windermere, Westmoreland. Looking West. T. Kennett-Barrington. 1913. Silurian.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803851.jp2&y=305&x=1779 Page&nbsp;65]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395003 P806687] || Silurian rocks scenery. Windermere, Westmoreland. Looking West. T. Kennett-Barrington. 1913. Silurian.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395004 P806688] || Silurian rocks scenery. Windermere, Westmoreland. Looking North. T. Kennett-Barrington. 1913. Silurian.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803851.jp2&y=305&x=1779 Page&nbsp;65]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395004 P806688] || Silurian rocks scenery. Windermere, Westmoreland. Looking North. T. Kennett-Barrington. 1913. Silurian.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395005 P806689] || Silurian stacks. Nr. St. Abb's Head. E.C. Martin. [Silurian.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803852.jp2&y=305&x=1780 Page&nbsp;66]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395005 P806689] || Silurian stacks. Nr. St. Abb's Head. E.C. Martin. [Silurian.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395006 P806690] || Section of quarry in Blakeway Hollow Lane, showing 'ballstone' occurring in stratified Wenlock Limestone. Much Wenlock. M.S. Johnstone. [Silurian.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803853.jp2&y=305&x=1781 Page&nbsp;67]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395006 P806690] || Section of quarry in Blakeway Hollow Lane, showing 'ballstone' occurring in stratified Wenlock Limestone. Much Wenlock. M.S. Johnstone. [Silurian.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395007 P806691] || Section of quarry in Blakeway Hollow Lane, showing 'ballstone' occurring in stratified Wenlock Limestone. Much Wenlock. M.S. Johnstone. [Silurian.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803853.jp2&y=305&x=1781 Page&nbsp;67]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395007 P806691] || Section of quarry in Blakeway Hollow Lane, showing 'ballstone' occurring in stratified Wenlock Limestone. Much Wenlock. M.S. Johnstone. [Silurian.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395008 P806692] || Section of quarry in Blakeway Hollow Lane, showing 'ballstone' occurring in stratified Wenlock Limestone. Much Wenlock. M.S. Johnstone. [Silurian.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803853.jp2&y=305&x=1781 Page&nbsp;67]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395008 P806692] || Section of quarry in Blakeway Hollow Lane, showing 'ballstone' occurring in stratified Wenlock Limestone. Much Wenlock. M.S. Johnstone. [Silurian.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395009 P806693] || 'Ballstone' in Wenlock Limestone. Nr. Much Wenlock. M.S. Johnstone. [Silurian.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803853.jp2&y=305&x=1781 Page&nbsp;67]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395009 P806693] || 'Ballstone' in Wenlock Limestone. Nr. Much Wenlock. M.S. Johnstone. [Silurian.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395010 P806694] || Section of Wenlock Limestone. Shadwell Rock. Much Wenlock. M.S. Johnstone. [Silurian.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803853.jp2&y=305&x=1781 Page&nbsp;67]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395010 P806694] || Section of Wenlock Limestone. Shadwell Rock. Much Wenlock. M.S. Johnstone. [Silurian.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395011 P806695] || Contorted strata. 70 ft. thick. Gleedon Hill, near Much Wenlock. M.S. Johnstone. [Silurian.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803853.jp2&y=305&x=1781 Page&nbsp;67]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395011 P806695] || Contorted strata. 70 ft. thick. Gleedon Hill, near Much Wenlock. M.S. Johnstone. [Silurian.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td></tr>
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</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Geologists%27_Association_%27green%27_album_1_-_index,_GA_%27Carreck_Archive%27&diff=46820&oldid=prev
Scotfot: /* Devonian */
2020-07-19T23:07:25Z
<p><span dir="auto"><span class="autocomment">Devonian</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 23:07, 19 July 2020</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wikitable"</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wikitable"</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394992 P806676] || Lower Limestone Shale. Devonian. Skrinkle Bay, Pembrokeshire. T. Kennett-Barrington. 1913. Devonian.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803849.jp2&y=305&x=1777 Page&nbsp;63]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394992 P806676] || Lower Limestone Shale. Devonian. Skrinkle Bay, Pembrokeshire. T. Kennett-Barrington. 1913. Devonian.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394993 P806677] || Contorted Devonian Rocks. South of Croyde Bay, Devonshire. J. Parker. 26.3.10. Devonian.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803849.jp2&y=305&x=1777 Page&nbsp;63]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394993 P806677] || Contorted Devonian Rocks. South of Croyde Bay, Devonshire. J. Parker. 26.3.10. Devonian.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394994 P806678] || Contorted Devonian Rocks. South of Croyde Bay, Devonshire. J. Parker. 26.3.10. Devonian.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803849.jp2&y=305&x=1777 Page&nbsp;63]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394994 P806678] || Contorted Devonian Rocks. South of Croyde Bay, Devonshire. J. Parker. 26.3.10. Devonian.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394995 P806679] || Old Red Sandstone overlain by Carboniferous breccia. Portishead, Somerset. T.W. Reader. 1919. Devonian.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803849.jp2&y=305&x=1777 Page&nbsp;63]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394995 P806679] || Old Red Sandstone overlain by Carboniferous breccia. Portishead, Somerset. T.W. Reader. 1919. Devonian.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394996 P806680] || Gorge of Logan Lee Burn through Basal Conglomerate of O.R.S. Pentland Hills, Midlothian. 31.7.27. Dixon Hewitt. Devonian.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803849.jp2&y=305&x=1777 Page&nbsp;63]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394996 P806680] || Gorge of Logan Lee Burn through Basal Conglomerate of O.R.S. Pentland Hills, Midlothian. 31.7.27. Dixon Hewitt. Devonian.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394997 P806681] || Natural steps formed by band of mudstone in Old Red Stone (nearly vertical). Old Castle Head, Pemblokeshire. H. Dixon Hewitt. 15.4.33. Devonian.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803849.jp2&y=305&x=1777 Page&nbsp;63]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394997 P806681] || Natural steps formed by band of mudstone in Old Red Stone (nearly vertical). Old Castle Head, Pemblokeshire. H. Dixon Hewitt. 15.4.33. Devonian.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394998 P806682] || O.R.S. conglomerate. Cushenden, N. Ireland. T. Shelford. Aug. 1935. Devonian.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803849.jp2&y=305&x=1777 Page&nbsp;63]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394998 P806682] || O.R.S. conglomerate. Cushenden, N. Ireland. T. Shelford. Aug. 1935. Devonian.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394999 P806683] || Overfolds in the cliffs on the N.E. side of Wild Pear Beach, Devonshire. G.M. Vevers. Easter 1922. [Devonian.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803850.jp2&y=305&x=1778 Page&nbsp;64]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394999 P806683] || Overfolds in the cliffs on the N.E. side of Wild Pear Beach, Devonshire. G.M. Vevers. Easter 1922. [Devonian.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395000 P806684] || 'Fucoids' on dip surface on the descent to Samson's Caves, Devonshire. G.M Davies. Easter 1922. [Devonian.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803850.jp2&y=305&x=1778 Page&nbsp;64]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395000 P806684] || 'Fucoids' on dip surface on the descent to Samson's Caves, Devonshire. G.M Davies. Easter 1922. [Devonian.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395001 P806685] || Devonian. Dip slope E. of Rillage Point, Devonshire. Undulations pitching to the West and fissures filled with calcite hading to the East. A.J. Bull. Easter 1922. [Devonian.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803850.jp2&y=305&x=1778 Page&nbsp;64]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395001 P806685] || Devonian. Dip slope E. of Rillage Point, Devonshire. Undulations pitching to the West and fissures filled with calcite hading to the East. A.J. Bull. Easter 1922. [Devonian.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395002 P806686] || Contorted Limestone Band in calcareous shale on the West side of Newberry Beach, Devonshire. G.M. Stockley. Easter 1922. [Devonian.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803850.jp2&y=305&x=1778 Page&nbsp;64]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=395002 P806686] || Contorted Limestone Band in calcareous shale on the West side of Newberry Beach, Devonshire. G.M. Stockley. Easter 1922. [Devonian.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Geologists%27_Association_%27green%27_album_1_-_index,_GA_%27Carreck_Archive%27&diff=46819&oldid=prev
Scotfot: /* Carboniferous */
2020-07-19T23:03:11Z
<p><span dir="auto"><span class="autocomment">Carboniferous</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 23:03, 19 July 2020</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wikitable"</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wikitable"</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394980 P806664] || Carboniferous Limestone Scenery. The Mumbles, Glamorganshire. T. Kennett-Barrington. 1913. Carboniferous.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803845.jp2&y=305&x=1773 Page&nbsp;59]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394980 P806664] || Carboniferous Limestone Scenery. The Mumbles, Glamorganshire. T. Kennett-Barrington. 1913. Carboniferous.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394981 P806665] || 'Marble Cliffs', Harlyn Bay, Cornwall. Folded limestone and slate beds. C.A. Stocken. Easter 14. Carboniferous.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803845.jp2&y=305&x=1773 Page&nbsp;59]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394981 P806665] || 'Marble Cliffs', Harlyn Bay, Cornwall. Folded limestone and slate beds. C.A. Stocken. Easter 14. Carboniferous.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394982 P806666] || Fossil Coal tree. Glasgow. E.C. Martin. Carboniferous.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803845.jp2&y=305&x=1773 Page&nbsp;59]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394982 P806666] || Fossil Coal tree. Glasgow. E.C. Martin. Carboniferous.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394983 P806667] || Fossil Coal tree. Glasgow. E.C. Martin. Carboniferous.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803845.jp2&y=305&x=1773 Page&nbsp;59]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394983 P806667] || Fossil Coal tree. Glasgow. E.C. Martin. Carboniferous.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394984 P806668] || Carboniferous Limestone. Waterlip, Somerset. J. Parker. 29.5.19. Carboniferous.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803845.jp2&y=305&x=1773 Page&nbsp;59]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394984 P806668] || Carboniferous Limestone. Waterlip, Somerset. J. Parker. 29.5.19. Carboniferous.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394985 P806669] || Lower Carboniferous. Ripple marked sandstone. Ardross, Fife, Scotland. P. McIntyre. 6.8.1903. Carboniferous.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803845.jp2&y=305&x=1773 Page&nbsp;59]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394985 P806669] || Lower Carboniferous. Ripple marked sandstone. Ardross, Fife, Scotland. P. McIntyre. 6.8.1903. Carboniferous.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394986 P806670] || Lower Carboniferous. Small anti-cline on shore. Ardross, Fife, Scotland. P. McIntyre. 5.8.1903. Carboniferous.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803845.jp2&y=305&x=1773 Page&nbsp;59]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394986 P806670] || Lower Carboniferous. Small anti-cline on shore. Ardross, Fife, Scotland. P. McIntyre. 5.8.1903. Carboniferous.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394987 P806671] || Carboniferous Limestone. View from Church Doors Bridge of Skrinkle Haven, looking over the Horse's Back to Tenby. Caldy Island beyond. H. Dixon-Hewitt. 15.4.33. [Carboniferous.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803846.jp2&y=305&x=1774 Page&nbsp;60]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394987 P806671] || Carboniferous Limestone. View from Church Doors Bridge of Skrinkle Haven, looking over the Horse's Back to Tenby. Caldy Island beyond. H. Dixon-Hewitt. 15.4.33. [Carboniferous.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394988 P806672] || Quarry in Ingletonian 'granite' nr. Horton-in-Ribblesdale, Yorks. H. Dixon-Hewitt. 12.8.33. [Carboniferous.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803846.jp2&y=305&x=1774 Page&nbsp;60]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394988 P806672] || Quarry in Ingletonian 'granite' nr. Horton-in-Ribblesdale, Yorks. H. Dixon-Hewitt. 12.8.33. [Carboniferous.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394989 P806673] || Folding. Carboniferous Limestone, Hambledon Quarry, nr. Skipton, Yorks. H. Dixon-Hewitt. 16.8.33. [Carboniferous.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803846.jp2&y=305&x=1774 Page&nbsp;60]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394989 P806673] || Folding. Carboniferous Limestone, Hambledon Quarry, nr. Skipton, Yorks. H. Dixon-Hewitt. 16.8.33. [Carboniferous.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394990 P806674] || Pitching fold in Coal Measures. W. of Saundersfoot Harbour, Pembrokeshire. H. Dixon Hewitt. 16.4.33. [Carboniferous.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803846.jp2&y=305&x=1774 Page&nbsp;60]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394990 P806674] || Pitching fold in Coal Measures. W. of Saundersfoot Harbour, Pembrokeshire. H. Dixon Hewitt. 16.4.33. [Carboniferous.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|-</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| GA013 || [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394991 P806675] || Fold in Millstone Grit. Tenby Beach, nr. Giskar Rock. H. Dixon Hewitt. 17.4.33. [Carboniferous.]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>| <ins style="font-weight: bold; text-decoration: none;">[https://pubs.bgs.ac.uk/publications.html?pubID=</ins>GA013<ins style="font-weight: bold; text-decoration: none;">#v=d&z=2&n=5&i=P803846.jp2&y=305&x=1774 Page&nbsp;60]</ins>|| [https://geoscenic.bgs.ac.uk/asset-bank/action/viewAsset?id=394991 P806675] || Fold in Millstone Grit. Tenby Beach, nr. Giskar Rock. H. Dixon Hewitt. 17.4.33. [Carboniferous.]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
</table>
Scotfot