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Summary
| Description |
English: Doweel Breccia Like the underlying Locharbriggs Sandstone Formation, the Doweel Breccia was formed in a Permian desert. However the breccia was not laid down by wind, but is the debris left by a flash flood following sudden intense rain. The contact between the reddish sandstone and the grey breccia is obvious in this view, taken in the rose garden in Castledykes Park. Sadly, the old quarry face is becoming overgrown, and unless some sort of action is taken it may not be long before the interesting geological features are completely obscured by ivy and other vegetation. |
| Date | |
| Source | From geograph.org.uk |
| Author | Anne Burgess |
| Attribution (required by the license) | Anne Burgess / Doweel Breccia / |
| 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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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 | 21:45, 28 February 2011 | | 640 × 427 (323 KB) | GeographBot | == {{int:filedesc}} == {{Information |description={{en|1=Doweel Breccia Like the underlying Locharbriggs Sandstone Formation, the Doweel Breccia was formed in a Permian desert. However the breccia was not laid down by wind, but is the debris left by a fla |
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