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The Screes

Cliff

Why this matters

The Screes is a sea cliff composed primarily of Carboniferous limestone, formed around 340 to 320 million years ago through the accumulation of marine sediments. It is notable for its exposure of durable limestone strata that have resisted erosion, contributing to the distinctive coastal topography of the Westmorland and Furness area.

What is recorded here

The Screes is shown as a cliff on the public map of Westmorland and Furness. The saved point is the map point or the centre of its mapped shape.
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