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Girdle Ness

Headland
Girdle Ness
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What is recorded here

Girdle Ness is a headland composed primarily of Old Red Sandstone, dating to the Devonian period, around 400 million years ago. It formed through sedimentation in a shallow marine or fluvial environment and is notable for its resistant rock formations that have withstood coastal erosion, contributing to the distinctive geography of the Aberdeen area.

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Photo: Mike Pennington · CC BY-SA 2.0