
mineral
Kfeldspar (Potassium Feldspar)
KAlSi3O8
AI-generated identification · may be incorrectHardness: 6 on the Mohs scale; Color: Typically pink, salmon-pink, or reddish; Luster: Vitreous to pearly; Crystal structure: Monoclinic or triclinic; Cleavage: Good in two directions at nearly 90 degrees; Specific gravity: 2.5-2.6
- Hardness
- 6 on the Mohs scale
- Color
- Typically pink, salmon-pink, or reddish
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6 on the Mohs scale; Color: Typically pink, salmon-pink, or reddish; Luster: Vitreous to pearly; Crystal structure: Monoclinic or triclinic; Cleavage: Good in two directions at nearly 90 degrees; Specific gravity: 2.5-2.6
Formation & geological history
Forms in igneous rocks like granite and syenite from cooling magma, as well as in pegmatites and metamorphic gneisses.
Uses & applications
Used in the manufacture of ceramics, porcelain, glass, and as a mild abrasive in scouring powders. Sometimes cut as a gemstone (such as amazonite or sunstone varieties).
Geological facts
Potassium feldspar is one of the most abundant mineral groups in the Earth's crust, making up about 12% of the crust by volume.
Field identification & locations
Easily identified in the field by its distinct pink to salmon color, blocky crystal form, and right-angle cleavage planes. Found worldwide in granitic terrains.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary