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

Potassium Feldspar (Orthoclase)

Orthoclase (KAlSi3O8)

Hardness: 6 on Mohs scale; Color: salmon pink to reddish-orange; Luster: vitreous to pearly; Crystal structure: Monoclinic; Cleavage: two planes at 90 degrees; Specific gravity: 2.55-2.63

Hardness
6 on Mohs scale
Color
salmon pink to reddish-orange
Luster
vitreous to pearly
Identified More mineral

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Physical properties

Hardness: 6 on Mohs scale; Color: salmon pink to reddish-orange; Luster: vitreous to pearly; Crystal structure: Monoclinic; Cleavage: two planes at 90 degrees; Specific gravity: 2.55-2.63

Formation & geological history

Formed in igneous rocks like granite and pegmatites through slow cooling of magma. It is a primary constituent of the Earth's crust.

Uses & applications

Used in the manufacture of glass and ceramics, as a filler in paint and rubber, and occasionally as a gemstone (moonstone variant).

Geological facts

Orthoclase is one of the ten index minerals of the Mohs scale of mineral hardness. The name is derived from the Greek for 'straight fracture', referring to its two cleavage planes at right angles.

Field identification & locations

Identify by its characteristic pink color and distinctive 90-degree cleavage planes. Commonly found in granitic mountain ranges worldwide.