File:Beach to the east of Osmington Mills - geograph.org.uk - 1322277.jpg

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Description
English: Beach to the east of Osmington Mills The rounded nodules on the beach are of calcite-cemented sandstone and come from the Bencliff Grit Formation which is found at the base of the cliffs. The ledges exposed by the low tide are of Osmington Oolite. This view is from a point on the beach close to the cascade. Geological information from Ian West's Geology of the Wessex Coast (Jurassic Coast) internet field guide
Date
Source From geograph.org.uk
Author Jim Champion
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Jim Champion / Beach to the east of Osmington Mills / 
Jim Champion / Beach to the east of Osmington Mills
Camera location50° 38′ 01.4″ N, 2° 22′ 30″ W  Heading=112° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location50° 38′ 01.1″ N, 2° 22′ 28″ W  Heading=112° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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Attribution: Jim Champion
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Beach to the east of Osmington Mills

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title: Beach to the east of Osmington Mills (English)
author name string: Jim Champion

50°38'1.39"N, 2°22'29.64"W

heading: 112 degree

24 May 2009

50°38'1.07"N, 2°22'27.84"W

heading: 112 degree

image/jpeg

30adc91a5a5f0b51e5bb44bc6f1b6e6825c3924c

106,140 byte

640 pixel

427 pixel

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Date/TimeThumbnailDimensionsUserComment
current20:08, 27 February 2011Thumbnail for version as of 20:08, 27 February 2011427 × 640 (104 KB)GeographBot== {{int:filedesc}} == {{Information |description={{en|1=Beach to the east of Osmington Mills The rounded nodules on the beach are of calcite-cemented sandstone and come from the Bencliff Grit Formation which is found at the base of the cliffs. The ledges

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