What is recorded here

Flass Knotts 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.

Flass Knotts is a sea cliff composed primarily of Carboniferous limestone, formed around 340 to 320 million years ago through the accumulation of marine sediments. The cliff is notable for its exposure of layered sedimentary rock, which provides insight into ancient tropical marine environments and is typical of the geological formations found in the region.

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