File:Carbonated Dyke - geograph.org.uk - 938526.jpg
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Size of this preview: 407 × 599 pixels. Other resolutions: 163 × 240 pixels | 435 × 640 pixels.
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Summary
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| Description |
English: Carbonated Dyke The gap in the dark tuffs is a dyke of basalt which has been partly altered by replacement of some of its minerals by carbonate minerals. Being weaker than the tuffs it has been differentially eroded. It can be traced as a pale band winding through the sandstones beyond. |
| Date | |
| Source | From geograph.org.uk |
| Author | Anne Burgess |
| Attribution (required by the license) | Anne Burgess / Carbonated Dyke / |
| Camera location |   | View this and other nearby images on: OpenStreetMap |  |
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_heading:90.00&language=en){kind=link}
| Object location | | View this and other nearby images on: OpenStreetMap | |
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_heading:90.00&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 | 06:05, 22 February 2011 | | 435 × 640 (266 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=Carbonated Dyke The gap in the dark tuffs is a dyke of basalt which has been partly altered by replacement of some of its minerals by carbonate minerals. Being weaker than the tuffs it has been diff |
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