dark gray to black, fine-grained, intrusive igneous rock that occurs in Essex County, Mass.; at Mount Royal, near Montreal; near Oslo, Nor.; at Roztoky, Czech Republic; and at Carclout, Scot. It contains plagioclase as the dominant feldspar, as well as orthoclase feldspar, augite, biotite, hornblende, olivine, and nepheline. As the proportion of nepheline increases, essexite grades into theralite.