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A wave cut platform is formed when the destructive waves hit the face of the cliff and cause undercutting between the high and low tide marks. This is a result of corrosion and hydraulic action it is called a wave-cut notch and the part of cliff above is called the overhang . This notch gets bigger over time and creates a small cave under the cliff. The overhang will eventually become unsupported and then it will collapses and the cliff begins to retreat. The boulders from the cliff will be carried away by the sea and will uncover a gently slopping wave-cut platform. As this process repeats itself the wave-cut platform will increase in size as the cliff retreats further. At high tide the wave-cut notch will slowly become smoother from erosion such as solution, attrition and corrosion although it will still have rock pools.

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