File:Seaweed covered groyne - geograph.org.uk - 792669.jpg
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| Description |
English: Seaweed covered groyne 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.
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 |
| Attribution (required by the license) | Evelyn Simak / Seaweed covered groyne / |
| Camera location |   | View this and other nearby images on: OpenStreetMap |  |
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_heading:315.00&language=en){kind=link}
| Object location | | View this and other nearby images on: OpenStreetMap | |
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_heading:315.00&language=en){kind=link}
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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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| current | 05:54, 20 February 2011 | | 640 × 480 (160 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=Seaweed covered groyne 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 mar |
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