File:Flow banding in igneous rock.jpg
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Summary
| Description | A rhyolite boulder near Carn Alw shows the characteristic pattern of swirling or parallel layers called flow banding. It was caused by the molten magma meeting a hard surface before cooling and setting - this would have taken place beneath the sea 470 million years ago. |
| Date | |
| Source | https://www.geograph.org.uk/photo/1450246 |
| Author | ceridwen - https://www.geograph.org.uk/profile/6699 |
| Permission (Reusing this file) |
https://www.geograph.org.uk/photo/1450246 |
| Attribution (required by the license) | ceridwen / Flow banding in igneous rock / |
| Camera 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 ceridwen 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: ceridwen
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File history
Click on a date/time to view the file as it appeared at that time.
| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 15:29, 15 February 2011 | | 640 × 480 (134 KB) | דקי |
File usage
The following 7 pages use this file:
- Dominant group/Geology
- User:Marshallsumter/Chemicals/Rocks
- User:Marshallsumter/Keynote lectures (draft)/Geology
- User:Marshallsumter/Radiation astronomy1/Particles
- User:Marshallsumter/Radiation astronomy2/Rocks
- User:Marshallsumter/Rocks/Rocky objects/Earth
- User:Marshallsumter/Volcanoes/Volcanic rocks
