File:Bennybeg Craig - geograph.org.uk - 1214766.jpg
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Bennybeg_Craig_-_geograph.org.uk_-_1214766.jpg (640 × 300 pixels, file size: 234 KB, MIME type: image/jpeg)
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Summary
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English: Bennybeg Craig This is one of a series of volcanic dykes caused by molten rock thrusting up through cracks in the crustal rocks: The solidified upwelling rock (in this case quartz-dolerite) is harder than the surrounding bedrock and weathers less over time leaving a cliff or wall of dolerite - Ideal for rock climbing. |
| Date | |
| Source | From geograph.org.uk |
| Author | Dr Richard Murray |
| Attribution (required by the license) | Dr Richard Murray / Bennybeg Craig / |
| Camera location |   | View this and other nearby images on: OpenStreetMap |  |
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| Object location | | View this and other nearby images on: OpenStreetMap | |
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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 Dr Richard Murray 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: Dr Richard Murray
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
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| current | 06:03, 26 February 2011 | | 640 × 300 (234 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=Bennybeg Craig This is one of a series of volcanic dykes caused by molten rock thrusting up through cracks in the crustal rocks: The solidified upwelling rock (in this case quartz-dolerite) is harde |
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