File:Layers of glacial sediments resting on chalk base - a closer view - geograph.org.uk - 613950.jpg

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English: Layers of glacial sediments resting on chalk base - a closer view. The pebble beach at Weybourne marks the start of the cliff section of the Norfolk coast that extends in easterly direction. This change in the character of the coastline is due to the properties of the chalk, which is harder to the east. The cliffs resting on this chalk base are composed of layers of glacial sediments of flints and fossils. For a more distant view of this particular section of cliff see > 613947; for a more distant view of the cliffs at Weybourne beach see > 613925
Date Taken on 16 November 2007
Source From geograph.org.uk
Author Evelyn Simak
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Evelyn Simak / Layers of glacial sediments resting on chalk base - a closer view / 
Evelyn Simak / Layers of glacial sediments resting on chalk base - a closer view
Camera location52° 56′ 58″ N, 1° 08′ 41″ E  Heading=157° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location52° 56′ 57″ N, 1° 08′ 41″ E  Heading=157° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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Attribution: Evelyn Simak
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current02:55, 7 February 2011Thumbnail for version as of 02:55, 7 February 2011480 × 640 (98 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Layers of glacial sediments resting on chalk base - a closer view The pebble beach at Weybourne marks the start of the cliff section of the Norfolk coast that extends in easterly direction. This ch

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