File:Cliff Strata at Weybourne - geograph.org.uk - 1478458.jpg

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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
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Ashley Dace / Cliff Strata at Weybourne / 
Ashley Dace / Cliff Strata at Weybourne
Camera location52° 56′ 58″ N, 1° 08′ 29″ E  Heading=180° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location52° 56′ 57″ N, 1° 08′ 29″ E  Heading=180° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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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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current11:26, 2 March 2011Thumbnail for version as of 11:26, 2 March 2011480 × 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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