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Rubha Dubh Chamais

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Rubha Dubh Chamais
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What is recorded here

Rubha Dubh Chamais is a basaltic sea cliff or coastal rock feature, likely formed during the Paleogene period through volcanic activity associated with the North Atlantic Igneous Province. It is notable for its potential association with the geological formations of the Scottish Highlands, which include extensive basalt flows and columnar jointing from ancient lava eruptions.

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Photo: Bob Jones · CC BY-SA 2.0