
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
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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.
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Epidote
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Mineral/Rock
Banded Gneiss (River Rock/Pebble)
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Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral