File:Flow banding in igneous rock.jpg

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Flow_banding_in_igneous_rock.jpg ‎(640 × 480 pixels, file size: 134 KB, MIME type: image/jpeg)

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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.
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Source https://www.geograph.org.uk/photo/1450246
Author ceridwen - https://www.geograph.org.uk/profile/6699
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(Reusing this file)		 https://www.geograph.org.uk/photo/1450246
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ceridwen / Flow banding in igneous rock / 
CC BY-SA 2.0
ceridwen / Flow banding in igneous rock
Camera location51° 58′ 16.39″ N, 4° 42′ 43.12″ W  Heading=90° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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Attribution: ceridwen
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current15:29, 15 February 2011Thumbnail for version as of 15:29, 15 February 2011640 × 480 (134 KB)דקי (talk | contribs)

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