File:Carboniferous Limestone - geograph.org.uk - 730739.jpg

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English: Carboniferous Limestone Great thicknesses of limestone of Carboniferous age (~350 million years) remain in the coastal hills in this area. Quarries on the south-facing slopes are no longer active, but serious extraction continues on the coast. The limestone is the result of accumulation of carbonate-rich muds from microscopic algae and shelly debris forming obvious fossils. Here the layers of the rock can be seen to dip steadily to the North.
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Source From geograph.org.uk
Author Jonathan Wilkins
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Jonathan Wilkins / Carboniferous Limestone / 
Jonathan Wilkins / Carboniferous Limestone
Camera location53° 16′ 52″ N, 3° 40′ 04″ W  Heading=315° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location53° 16′ 52″ N, 3° 40′ 04″ W  Heading=315° 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: Jonathan Wilkins
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current07:30, 19 February 2011Thumbnail for version as of 07:30, 19 February 2011640 × 480 (99 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Carboniferous Limestone Great thicknesses of limestone of Carboniferous age (~350 million years) remain in the coastal hills in this area. Quarries on the south-facing slopes are no longer active, b

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