File:Frozen spoil, Newbridge ball clay quarry - geograph.org.uk - 1654551.jpg
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Summary[edit]
| Description |
English: Frozen spoil, Newbridge ball clay quarry The spoil is predominantly lignite. It looks and feels like fine shale, soft underfoot where not frozen. In the Bovey Basin layers of lignite occur between the layers of clay and other minerals. In the past, lignite was used as a fuel to a minor extent. Here, a spoil heap appears to be in the course of formation, backfilling over part of the quarry, and looking set to overtop natural ground level. In the distance is Dartmoor, with Haytor, centre. |
| Date | |
| Source | From geograph.org.uk |
| Author | Robin Stott |
| Attribution (required by the license) | Robin Stott / Frozen spoil, Newbridge ball clay quarry / |
| 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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_heading:270.00&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 Robin Stott 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: Robin Stott
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
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| current | 21:02, 4 March 2011 | | 640 × 480 (398 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=Frozen spoil, Newbridge ball clay quarry The spoil is predominantly lignite. It looks and feels like fine shale, soft underfoot where not frozen. In the Bovey Basin layers of lignite occur between t |
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