Gabbro is a dark-colored, coarse-grained igneous rock that primarily consists of plagioclase feldspar and pyroxene. It forms when magma cools slowly beneath the Earth's surface, resulting in large crystals that are visible to the naked eye. This rock is a key component in understanding the processes of igneous rock formation and classification, as it represents a type of intrusive igneous rock that crystallizes from basaltic magma.
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