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coasts - Coggle Diagram
coasts
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subaerial process
mechanical
freeze thaw weathering.
freeze thaw weathering is where water gets into cracks in a cliff face. then, in the night, the water freezes and expands. this opens the crack up and can break bits of rock away from the cliff.
chemical
acid rain
acod rain is rain with a ph below 7. it can react with the rock on the cliff side especially if it is a weaker type of rock such as chalk or clay.
biological
plant roots
plant roots can cause damage to a coast as they can borrow deep into the ground pushing bits of rock apart from each other.
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there are different types of austlines that can lead to different shaped coasts with different features.
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sediment cells
A sediment cell is a largely self-contained stretch of coastline. They are regarded as closed systems as sediment is not usually transferred from one to the other. In reality,
some sediment does get transferred between neighbouring cells. Each sediment major cell typically has many smaller sub-cells.
the rock cycle.
types of rock
metamorphic
sedimentry rock is then buried under more pressure and heat as it falls closed towards the upper mantle of the earth. is therefore much stronger.
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sedimentry
bits of sedimentary rock found on the upper crust of the earth. compressed by little pressure as they are on top of most the crust
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igneous.
pushd into the mantle and melts. can then come bacl to the surface through volcanic activity. the strongest type of rock. examples can include granite and marble.
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