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Coast Revision (The Jurassic Coast (Durlston (Headland) (Formed when the…
Coast Revision
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Weathering
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Chemical Weathering
the erosion or disintegration of rocks, building materials, etc., caused by chemical reactions (chiefly with water and substances dissolved in it) rather than by mechanical processes.
Biological weathering
Biological weathering is the weakening and subsequent disintegration of rock by plants, animals and microbes.
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Landforms
Deposition
Spit
The longshore drift continues perpendicularly to move down the coastline even when the headland shape changes causing a saltmarsh to be formed behind the spit
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Erosion
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Cliffs
A steep rock face, especially at the edge of the sea.
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Wave Cut Platform
A flat area in front of a cliff, just below the low tide mark. These were formed when the waves eroded the cliff, but left a flat platform behind.
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Cave
As the waves continue to grind away at the crack, it begins to open up to form a cave.
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Stack
The base of the arch continually becomes wider through further erosion, until its roof becomes too heavy and collapses into the sea. This leaves a stack
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Erosion
Types of Erosion
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Attrition
Waves smash rocks and pebbles on the shore into each other, and they break and become smoother.
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Hydraulic Action
Air may become trapped in joints and cracks on a cliff face. When a wave breaks, the trapped air is compressed which weakens the cliff and causes erosion
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