What is recorded here

Pisgah is shown as a cliff on the public map of Cumberland. The saved point is the map point or the centre of its mapped shape.

Pisgah is a sea cliff composed primarily of Silurian-age sandstone, formed through sedimentation and subsequent uplift during the Caledonian orogeny. It is notable for its exposure of ancient marine sediments and its role in illustrating regional geological history along Cumberland’s coast.

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