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compare Weathering, Erosion, and Deposition.

The processes by which rock is broken into smaller pieces by the action of the weather. There are different types of weathering, there is freeze thaw weathering, biological weathering and chemical weathering.

Freeze-thaw weathering

Freeze-thaw weathering occurs when rocks are porous (contain holes) or permeable (allow water to pass through).

Biological weathering

Plants and animals can also have an effect on rocks. Roots burrow down, weakening the structure of the rock until it breaks away.

Chemical weathering

Rainwater and seawater can be a weak acid. If a coastline is made up of rocks such as limestone or chalk, over time they can become dissolved by the acid in the water.

Erosion is the wearing away of rock along the coastline. Destructive waves are responsible for erosion on the coastline. There are four types of erosion:

When the sea loses energy, it drops the material it has been carrying. This is known as deposition. Deposition can occur on coastlines that have constructive waves.

Factors leading to deposition include:

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folds are formed when heat and pressure is applied to the rock. the higher the temperature, the more pliable rocks become. folds are more likely to occur when the deformation caused by the compression is applied slowly. faults are defined as the displacement of rock that were once connected along a fault line.

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