File:St Martha on the Hill, Chilworth - geograph.org.uk - 432885.jpg
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Summary
| Description |
English: St Martha on the Hill, Chilworth St Martha's Hill is capped with Carstone. This is a sandstone of the Folkestone Sands deposited around 100 million years ago. It was hardened when water with iron in it percolated downwards to form an iron oxide called limonite. Much of exterior of the church has been faced with locally quarried Carstone whose rusty colour can be seen in this photograph. Folkestone Sands in their less hardened form can be seen in one of the Geographs for SU9948. |
| Date | |
| Source | From geograph.org.uk |
| Author | David Kemp |
| Attribution (required by the license) | David Kemp / St Martha on the Hill, Chilworth / |
| Camera location |   | View this and other nearby images on: OpenStreetMap |  |
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_heading:45.00&language=en){kind=link}
| Object location | | View this and other nearby images on: OpenStreetMap | |
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_heading:45.00&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 David Kemp 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: David Kemp
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File history
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 09:03, 4 February 2011 | | 640 × 480 (52 KB) | GeographBot | == {{int:filedesc}} == {{Information |description={{en|1=St Martha on the Hill, Chilworth St Martha's Hill is capped with Carstone. This is a sandstone of the Folkestone Sands deposited around 100 million years ago. It was hardened when water with iron in |
File usage
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