File:Dumblehole Brook - geograph.org.uk - 1202707.jpg
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| Description |
English: Dumblehole Brook The brook is running deep beneath the surrounding land. It has cut down to the new level of the river, which has been much larger since the Teme was diverted this way in glacial times. The dingle was formed by a retreating waterfall - the falls are behind The Dumblehole ("Dumbleholes Farm" according to the Ordnance Survey) at SO52697020.
The photograph was taken from the remains of a footbridge which carried a footpath around a ford at Dumblehole. The ford was filled in 1973, one plank of the now obsolete bridge remains. |
| Date | |
| Source | From geograph.org.uk |
| Author | Richard Webb |
| Attribution (required by the license) | Richard Webb / Dumblehole Brook / |
| 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}
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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 Richard Webb 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: Richard Webb
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 03:13, 26 February 2011 | | 640 × 480 (164 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=Dumblehole Brook The brook is running deep beneath the surrounding land. It has cut down to the new level of the river, which has been much larger since the Teme was diverted this way in glacial tim |
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