The way in which temperature leads to weathering of rocks is as follows: Rocks expand and contract when they are heated and cooled which cause them to break (option C).
Rock weathering is the mechanical or chemical breaking down of rocks in situ by weather or other causes.
Once a rock has been broken down, a process called erosion transports the bits of rock and minerals away. Water, acids, salt, plants, animals, and changes in temperature are all agents of weathering and erosion.
Changes in temperature cause rock to expand (with heat) and contract (with cold). As this happens over and over again, the structure of the rock weakens. Over time, the rock crumbles.
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