Granodiorite is an igneous rock that is similar to granite but contains a higher percentage of plagioclase feldspar. It typically has a coarse-grained texture, composed mainly of quartz, feldspar, and biotite or hornblende. Granodiorite forms from the slow cooling of magma beneath the Earth's surface, allowing large crystals to develop. This rock is commonly found in continental crust and is often associated with mountain-building processes. Granodiorite is used in construction and as a decorative stone due to its durability and attractive appearance. It can be found in various locations, including Sierra Nevada in California and the Andes in South America.