Wester Keolka, Shetland Islands

Crags at Easter Keolka

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The crags are composed of highly sheared Lewisian gneiss, probably at least 1.8 billion years old but reworked around 500 million years ago.

Uploaded to Geograph by Tim Harrison on 20 July 2010

Creative Commons License Photo © Tim Harrison, 20 July 2010. Licensed for reuse under this Creative Commons licence

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