Why this matters
Rubha Redegich is a headland composed primarily of Devonian-age sandstone, formed through the deposition and lithification of sediments in a shallow marine environment. Its notable position along the coast contributes to the distinctive topography of the Argyll and Bute region.
What is recorded here
Rubha Redegich is shown as a headland on the public map of Argyll and Bute. The saved point is the map point or the centre of its mapped shape.
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