Why this matters
Tridley Point is a headland composed primarily of Silurian greywacke and volcanic rocks, formed around 440–420 million years ago through sedimentation and volcanic activity. It is notable for its resistant rock formations that have withstood coastal erosion, contributing to the distinctive landscape of the Westmorland and Furness coastline.
What is recorded here
Tridley Point is shown as a headland 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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