File:Cliff Strata at Weybourne - geograph.org.uk - 1478458.jpg
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DescriptionCliff Strata at Weybourne - geograph.org.uk - 1478458.jpg |
English: Cliff Strata at Weybourne The chalk is the bottom white layer, the next is flint and pebbles. These have been eroded from the chalk and then deposited ontop of it. This layer also contains bivalve fossils.
Then there is clays and sands from the glacial deposits. |
Date | Taken on 4 September 2009 |
Source | From geograph.org.uk |
Author | Ashley Dace |
Attribution (required by the license) InfoField | Ashley Dace / Cliff Strata at Weybourne / |
InfoField | Ashley Dace / Cliff Strata at Weybourne |
Camera location | 52° 56′ 58″ N, 1° 08′ 29″ E | View this and other nearby images on: OpenStreetMap | 52.949520; 1.141300 |
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Object location | 52° 56′ 57″ N, 1° 08′ 29″ E | View this and other nearby images on: OpenStreetMap | 52.949070; 1.141300 |
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This image was taken from the Geograph project collection. See this photograph's page on the Geograph website for the photographer's contact details. The copyright on this image is owned by Ashley Dace and is licensed for reuse under the Creative Commons Attribution-ShareAlike 2.0 license.
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This file is licensed under the Creative Commons Attribution-Share Alike 2.0 Generic license.
Attribution: Ashley Dace
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current | 11:26, 2 March 2011 | 480 × 640 (99 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=Cliff Strata at Weybourne The chalk is the bottom white layer, the next is flint and pebbles. These have been eroded from the chalk and then deposited ontop of it. This layer also contains bivalve f |
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