When granite melts and then solidifies, it typically forms a type of igneous rock known as granite's molten counterpart, which is often referred to as "granite magma." Upon cooling, this magma can crystallize into a rock similar to granite but may exhibit different mineral compositions or textures, depending on the conditions of cooling and the presence of other materials. If the cooling occurs slowly beneath the Earth's surface, it will form a coarse-grained rock, whereas rapid cooling can lead to a finer-grained texture.
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