Rock Identifier
Feldspar (Orthoclase / Alkali Feldspar) (KAlSi3O8 (Potassium Feldspar / Orthoclase)) — mineral
mineral

Feldspar (Orthoclase / Alkali Feldspar)

KAlSi3O8 (Potassium Feldspar / Orthoclase)

Hardness: 6 on Mohs scale. Color: Salmon-pink, reddish-brown, tan, to orange. Luster: Vitreous to pearly on cleavage faces. Cleavage: Two directions intersecting at or near 90 degrees. Crystal system: Monoclinic/Triclinic. Specific gravity: 2.56 - 2.58.

Hardness
6 on Mohs scale
Color
Salmon-pink, reddish-brown, tan, to orange
Luster
Vitreous to pearly on cleavage faces
Identified More mineral
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Physical properties

Hardness: 6 on Mohs scale. Color: Salmon-pink, reddish-brown, tan, to orange. Luster: Vitreous to pearly on cleavage faces. Cleavage: Two directions intersecting at or near 90 degrees. Crystal system: Monoclinic/Triclinic. Specific gravity: 2.56 - 2.58.

Formation & geological history

Forms during the crystallization of igneous rocks (like granite and pegmatite) and metamorphic rocks. It crystallizes from silicate magma at high temperatures and pressures deep within the Earth's crust.

Uses & applications

Used extensively in the manufacture of ceramics, porcelain, enamel, and glass. High-quality transparent or chatoyant varieties (like moonstone or sunstone) are cut as gemstones. Fine powders are used as abrasives.

Geological facts

Feldspars are the most abundant group of minerals in the Earth's continental crust, making up roughly 60% of terrestrial rocks. Pink to reddish feldspars owe their color to micro-inclusions of iron oxide (hematite).

Field identification & locations

Identified by its distinctive salmon-pink to reddish tint, vitreous luster, and two prominent cleavage planes meeting at nearly right angles. Commonly found worldwide in granitic terrains, gravel beds, and pegmatite deposits.