File:Glacial erratics - geograph.org.uk - 1453615.jpg
Glacial_erratics_-_geograph.org.uk_-_1453615.jpg (640 × 480 pixels, file size: 81 KB, MIME type: image/jpeg)
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editDescriptionGlacial erratics - geograph.org.uk - 1453615.jpg |
English: Glacial erratics The size of some of the erratics that litter the island is quite awesome! Gwion is a useful scale marker in this image of a cluster of rather angular granite erratics which are up to 5m maximum dimension. In this location it is difficult to imagine any agent apart from a glacier that could move rocks this size. A rough calculation suggests that the larger of these is around twice the payload of a Chinook helicopter! |
Date | |
Source | From geograph.org.uk |
Author | Jonathan Wilkins |
Attribution (required by the license) InfoField | Jonathan Wilkins / Glacial erratics / |
InfoField | Jonathan Wilkins / Glacial erratics |
Camera location | 53° 15′ 16″ N, 9° 40′ 49″ W | View this and other nearby images on: OpenStreetMap | 53.254450; -9.680300 |
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Object location | 53° 15′ 16″ N, 9° 40′ 49″ W | View this and other nearby images on: OpenStreetMap | 53.254450; -9.680300 |
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Licensing
editThis 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 Jonathan Wilkins 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: Jonathan Wilkins
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This file, which was originally posted to
geograph.org.uk, was reviewed on 14 December 2018 by reviewer Taivo, who confirmed that it was available there under the stated license on that date.
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current | 05:21, 2 March 2011 | 640 × 480 (81 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=Glacial erratics The size of some of the erratics that litter the island is quite awesome! Gwion is a useful scale marker in this image of a cluster of rather angular granite erratics which are up t |
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