File:Chalk rafts - geograph.org.uk - 792996.jpg
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English: Chalk rafts The white chalk rafts seen in the cliff section on the approach to and below Wood Hill were shaped by ice, moving from the north north west and raising up to 40 metres above beach level. The chalk is composed of calcium carbonate from the remains of microscopic marine organisms that once lived in a warm shallow sea which covered this area between 62 and 132 million years ago. Layers of flint pebbles can be seen embedded in the chalk. http://www.chesterfieldlodge.fsnet.co.uk/Geology/west%20runton-east%20runton.htm
http://www.museums.norfolk.gov.uk/default.asp?document=400.500.100.025 Erosion is evidenced by the heaps of sand and other materials accumulated at the cliff base, due to recent slides. |
| Date | |
| Source | From geograph.org.uk |
| Author | Evelyn Simak |
| Attribution (required by the license) | Evelyn Simak / Chalk rafts / |
| Camera location |   | View this and other nearby images on: OpenStreetMap |  |
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| Object location | | View this and other nearby images on: OpenStreetMap | |
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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 Evelyn Simak 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: Evelyn Simak
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
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| current | 04:22, 20 February 2011 | | 640 × 480 (189 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=Chalk rafts The white chalk rafts seen in the cliff section on the approach to and below Wood Hill were shaped by ice, moving from the north north west and raising up to 40 metres above beach level. |
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