File:Quarry entrance, Gurney Slade - geograph.org.uk - 1253956.jpg

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Quarry_entrance,_Gurney_Slade_-_geograph.org.uk_-_1253956.jpg(640 × 495 pixels, file size: 126 KB, MIME type: image/jpeg)

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Description
English: Quarry entrance, Gurney Slade From the west in Gurneyslade Bottom.

"The region around Gurney Slade and Emborough is geologically quite complex, being located at the eastern end of the Pen Hill Pericline, one of the four major up-folds on Mendip. To the east the Carboniferous Limestone plunges downwards disappearing beneath the Upper Carboniferous Quartzitic Sandstone and the Coal Measures"

The above was copied from: http://www.bgs.ac.uk/mendips/localities/gurneyslade.html
Date
Source From geograph.org.uk
Author Maurice Pullin
Camera location51° 14′ 30″ N, 2° 32′ 05″ W  Heading=45° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location51° 14′ 32″ N, 2° 32′ 02″ W  Heading=45° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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w:en:Creative Commons
attribution share alike
This file is licensed under the Creative Commons Attribution-Share Alike 2.0 Generic license.
Attribution: Maurice Pullin
You are free:
  • to share – to copy, distribute and transmit the work
  • to remix – to adapt the work
Under the following conditions:
  • attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
  • share alike – If you remix, transform, or build upon the material, you must distribute your contributions under the same or compatible license as the original.

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current20:53, 26 February 2011Thumbnail for version as of 20:53, 26 February 2011640 × 495 (126 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Quarry entrance, Gurney Slade From the west in Gurneyslade Bottom. "The region around Gurney Slade and Emborough is geologically quite complex, being located at the eastern end of the Pen Hill Pe

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