Stair Hole
Stair Hole, less than half a mile away, is an infant cove which suggests what Lulworth Cove would have looked like a few hundred thousand years ago. The sea has made a gap in the Portland and Purbeck limestone here, as well as small arch. The sea has made its way through to the Wealdon clays and begun eroding them. The clay shows obvious signs of slumping, and is eroding very rapidly. Stair Hole shows one of the best examples of limestone folding (the Lulworth crumple) in the world, caused by movements in the Earth's crust (tectonics) millions of years ago. Folding can also be seen at nearby Durdle Door and at Lulworth cove itself.
Read more about this topic: Lulworth Cove
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