
mineral
Orthoclase Feldspar
KAlSi3O8 (Potassium Aluminum Silicate)
Hardness: 6.0 on Mohs scale; Color: Pink, flesh-red, tan, or yellowish-white; Luster: Vitreous to pearly; Crystal System: Monoclinic; Cleavage: Two directions meeting at 90 degrees; Specific Gravity: 2.55-2.63.
- Hardness
- 6
- Color
- Pink, flesh-red, tan, or yellowish-white
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6.0 on Mohs scale; Color: Pink, flesh-red, tan, or yellowish-white; Luster: Vitreous to pearly; Crystal System: Monoclinic; Cleavage: Two directions meeting at 90 degrees; Specific Gravity: 2.55-2.63.
Formation & geological history
Forms primarily in igneous rocks such as granite and syenite through the cooling of silica-rich magma; also found in metamorphic rocks like gneiss and in sedimentary arkose sandstones.
Uses & applications
Major ingredient in the manufacture of glass and ceramics (porcelain, floor tiles, and sanitary ware). Rare clear varieties are used as gemstones (Moonstone).
Geological facts
Orthoclase is the defining mineral for level 6 on the Mohs scale of mineral hardness. The name comes from the Greek for 'straight fracture,' referring to its two cleavage planes at right angles to each other.
Field identification & locations
Identifiable by its blocky shape, pearly luster on cleavage faces, and pinkish-tan color. Look for parallel lines (exsolution lamellae) on surface faces. Extremely common in continental crust worldwide.
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