File:And...^ - geograph.org.uk - 409728.jpg
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And...^_-_geograph.org.uk_-_409728.jpg (640 × 480 pixels, file size: 108 KB, MIME type: image/jpeg)
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Summary[edit]
| Description |
English: And...? A fine speciment! View towards Westnewton. The Cheviot hills are very old, having been formed about 400 million years ago from magma. They have been smoothed and rounded by the action of ice and the characteristic rolling hills can be seen here. |
| Date | |
| Source | From geograph.org.uk |
| Author | Lisa Jarvis |
| Attribution (required by the license) | Lisa Jarvis / And...? / |
| Camera location |   | View this and other nearby images on: OpenStreetMap |  |
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_heading:180.00&language=en){kind=link}
| Object location | | View this and other nearby images on: OpenStreetMap | |
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_heading:180.00&language=en){kind=link}
Licensing[edit]
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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 Lisa Jarvis 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: Lisa Jarvis
- 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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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 20:44, 3 February 2011 | | 640 × 480 (108 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=And...? A fine speciment! View towards Westnewton. The Cheviot hills are very old, having been formed about 400 million years ago from magma. They have been smoothed and rounded by the action of ice |
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