Why this matters
Strathcashell Point is a coastal headland composed primarily of Silurian greywacke and volcanic rocks, formed around 440 to 420 million years ago during the Caledonian orogeny. The area is notable for its resistant rock formations that have withstood erosion, creating a prominent feature along the coast.
What is recorded here
Strathcashell Point is shown as a headland on the public map of Stirling. The saved point is the map point or the centre of its mapped shape.
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