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The process of which freeze-thaw or physical weathering takes place is rather simple.

Firstly, water would get into cracks on a rock or hard material, and overnight, it would freeze.

Secondly, because when water freezes, it expands, it therefore forces itself further into the rock; the crack is made larger.

Lastly, this would created more space inside the rock, for more water to end up inside, and join in with the freeze-thaw, until finally, the rock would break.

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