a feldspar mineral, calcium aluminosilicate (CaAl₂Si₂O₈), that occurs as white or grayish, brittle, glassy crystals. Primarily a rock-forming mineral, it is used in the manufacture of glass and ceramics. Anorthite occurs in basic igneous rocks, as at Trentino, Italy; Södermanland, Swed.; Tamil Nadu, India; Miyake, Japan; and Franklin, N.J. For detailed physical properties, see feldspar (table).

The feldspar minerals are mixtures of sodium, potassium, and calcium aluminosilicates; they belong to a ternary system in which any mineral may be classed by its percentage of each of three pure compounds, called end-members: sodium aluminosilicate, potassium aluminosilicate, and calcium aluminosilicate. Anorthite is the calcium-bearing end-member of the system; its symbol is An.

Anorthite and the sodium-bearing end-member of the system, albite (NaAlSi₃O₈), form a solid-solution series in which the two intermingle; thus, in nature there is a continuous chemical variation between the two compounds. Any member of this series is called a plagioclase.