Orthoclase Feldspar
Orthoclase (KAlSi3O8)
Rock Type: mineral

Physical Properties
Hardness: 6 on Mohs scale; Color: Pink, flesh-colored, or yellowish-tan; Luster: Vitreous to pearly; Crystal Structure: Monoclinic; Cleavage: Two planes at right angles (90 degrees); Specific Gravity: 2.55-2.63
Formation & Geological History
Formed as a primary constituent in igneous rocks like granite and syenite through the cooling of magma. It can also be found in high-grade metamorphic rocks and as grains in sedimentary rocks.
Uses & Applications
Used in the manufacture of glass and ceramics (porcelain); sometimes used as a mild abrasive in scouring pads. High-quality varieties like moonstone are used in jewelry.
Geological Facts
Orthoclase is one of the ten index minerals on 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 in the field by its distinct 90-degree cleavage, flesh-like color, and pearly luster. Found worldwide in granitic batholiths and pegmatites. Collectors look for well-defined crystal faces.
Identified on: 4/29/2026
Mode: Standard