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Sea stacks are geological formations found along erosional coastlines. They are remnants of rock left behind after wave erosion has worn away the surrounding land. These isolated pinnacles stand on wave-cut platforms, which are smooth, horizontal surfaces created by wave action at the base of sea cliffs.

The formation of sea stacks is a continuous process. Initially, erosion can create sea arches. When these arches eventually collapse, a sea stack is left standing. Over time, further erosion will wear down the sea stack until it disappears, leaving only the wave-cut platform and the coastal cliff. The rate of erosion depends on the type of rock and the energy of the waves.123

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