What is recorded here

Haw Bank is shown as a cliff on the public map of North Yorkshire. The saved point is the map point or the centre of its mapped shape.

Haw Bank is a sea cliff composed primarily of Jurassic limestone, formed around 150 to 180 million years ago through the accumulation of marine sediments. It is notable for its exposure of the Cleveland Ironstone Formation, which historically supported local ironstone mining and provides important insights into the region's geological and industrial past.

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