Lavernock Point

Headland

Why this matters

Lavernock Point is a headland composed mainly of Carboniferous limestone, formed around 340 million years ago through the accumulation of marine sediments. It is notable for its coastal erosion features and as a key geographical landmark in the Vale of Glamorgan.

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What is recorded here

Lavernock Point is shown as a headland on the public map of Vale of Glamorgan. The saved point is the map point or the centre of its mapped shape.

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