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This is a ropy flow-structure on the lower, inner surface of a large, flattened vesicle at the top of the Farne Islands Dolerite Sill. It is a part of the Whin Sill-swarm and was emplaced within Carboniferous rocks. @BritGeoSurvey #Igneous #Bamburgh
earthwise.bgs.ac.uk/index.php/Earl…

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