This interesting dolerite boulder, which sits close to Lion Rock, exhibits quite regular jointing.
The Triassic sedimentary rocks weather in quite interesting ways. I assume this is caused by the action of salt and seawater over time. Some of these boulders end up looking like enormous sponges.
The cliffs at the eastern end of the bay carry a warning sign at the top suggesting that people stay away from the edges. When you get a good look at them from beneath, you can see why; they are very badly eroded, and obviously large pieces of cliff have fallen in the past, some look quite recent. I expect to arrive at the bay one day and find these cliffs remodelled significantly.
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