File:Chalk outcrops on the foreshore - geograph.org.uk - 792673.jpg

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Chalk outcrops on the foreshore

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Description
English: Chalk outcrops on the foreshore Low water has exposed outcrops of chalk, a characteristic feature for this section of coastline. 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. On the low foreshore, flint circles and nodules can be observed along with paramoudras, also known as pot stones. A stone and pebble spit can be seen in the background, extending even further out into the sea.

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
Date
Source From geograph.org.uk
Author Evelyn Simak
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Evelyn Simak / Chalk outcrops on the foreshore / 
Evelyn Simak / Chalk outcrops on the foreshore
Camera location52° 56′ 36″ N, 1° 14′ 47″ E  Heading=337° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location52° 56′ 39″ N, 1° 14′ 45″ E  Heading=337° 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: Evelyn Simak
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current04:22, 20 February 2011Thumbnail for version as of 04:22, 20 February 2011480 × 640 (175 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Chalk outcrops on the foreshore Low water has exposed outcrops of chalk, a characteristic feature for this section of coastline. The chalk is composed of calcium carbonate from the remains of micros

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