Yes, mineral size can affect the rate of cooling in igneous rocks. Larger mineral crystals typically form when magma cools slowly, allowing more time for crystal growth, which occurs in intrusive rocks. Conversely, smaller crystals result from rapid cooling, often seen in extrusive rocks like basalt, where lava solidifies quickly upon exposure to the surface environment. Thus, the size of the minerals can provide insights into the cooling history of the rock.
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