What is recorded here

Felicia Crags is shown as a cliff on the public map of Northumberland. The saved point is the map point or the centre of its mapped shape.

Felicia Crags is a sea cliff composed primarily of Carboniferous limestone, formed around 340 million years ago through the accumulation of marine sediments. The crags are notable for their coastal exposure of durable limestone strata, which resist erosion and create a striking geological feature along Northumberland's coastline.

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