File:Cliff erosion - geograph.org.uk - 792987.jpg

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Cliff_erosion_-_geograph.org.uk_-_792987.jpg (640 × 459 pixels, file size: 188 KB, MIME type: image/jpeg)

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Cliff erosion

Summary

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Description
English: Cliff erosion 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 to the 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. Erosion is evidenced by the heaps of sand and other materials accumulated at the cliff base, due to recent slides.
Date Taken on 7 May 2008
Source From geograph.org.uk
Author Evelyn Simak
Attribution
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InfoField
Evelyn Simak / Cliff erosion / 
Evelyn Simak / Cliff erosion
Camera location52° 56′ 20″ N, 1° 16′ 14″ E  Heading=270° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location52° 56′ 20″ N, 1° 16′ 09″ E  Heading=270° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

Licensing

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w:en:Creative Commons
attribution share alike
This file is licensed under the Creative Commons Attribution-Share Alike 2.0 Generic license.
Attribution: Evelyn Simak
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Date/TimeThumbnailDimensionsUserComment
current04:25, 20 February 2011Thumbnail for version as of 04:25, 20 February 2011640 × 459 (188 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Cliff erosion 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 to the west and raising up to 40 metres above beach lev

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