An igneous rock texture in which the crystals are roughly equal in size and large enough so that individual minerals can be identified with the unaided eye
An igneous rock texture characterized by two distictively different crystal sizes. The larger crystals are called phenocrysts, and the matrix of smaller crystals is termed the groundmass
A very coarse-grained igneous rock (typically granite) commonly found as a dike associated with a large mass of plutonic rock that has smaller crystals. Crystallization in a water-rich enviornment is believed to be responible for the very large crystals