File:Cross Geo, Clibberswick - geograph.org.uk - 8675.jpg
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Size of this preview: 364 × 599 pixels. Other resolutions: 146 × 240 pixels | 389 × 640 pixels.
Original file (389 × 640 pixels, file size: 228 KB, MIME type: image/jpeg)
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Summary
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| Description |
English: Cross Geo, Clibberswick. This is another part of the Unst ophiolite. The black pebbles are serpentinite, and the white rocks are sea-washed talc, which is formed by alteration of the serpentinite. The talc is quarried for industrial use. |
| Date | |
| Source | From geograph.org.uk |
| Author | Anne Burgess |
| Attribution (required by the license) | Anne Burgess / Cross Geo, Clibberswick / |
| Camera location |   | View this and other nearby images on: OpenStreetMap |  |
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_heading:247.00&language=en){kind=link}
| Object location | | View this and other nearby images on: OpenStreetMap | |
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_heading:247.00&language=en){kind=link}
Licensing
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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 Anne Burgess 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: Anne Burgess
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 01:10, 30 January 2010 | | 389 × 640 (228 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=Cross Geo, Clibberswick. This is another part of the Unst ophiolite. The black pebbles are serpentinite, and the white rocks are sea-washed talc, which is formed by alteration of the serpentinite. T |
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