Potassium Feldspar (Orthoclase)
KAlSi3O8
Rock Type: mineral

Physical Properties
Hardness: 6 on Mohs scale; Color: Pinkish-orange (salmon); Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Two directions at 90 degrees; Specific Gravity: 2.55-2.63.
Formation & Geological History
Forms in igneous rocks like granite and syenite through the cooling of silica-rich magma; also found in metamorphic rocks (gneiss) and some sedimentary sandstones (arkose).
Uses & Applications
Used primarily in the manufacture of glass and ceramics (porcelain), as a filler in paints and plastics, and occasionally as a gemstone (moonstone variety).
Geological Facts
Feldspar is the most abundant mineral group in the Earth's crust. The pink color in this specimen is often caused by trace amounts of iron or hematite inclusions.
Field Identification & Locations
Identify in the field by its distinct salmon-pink color, blocky cleavage, and its ability to scratch glass but be scratched by a steel file. Commonly found in granitic mountainous regions.
Identified on: 5/10/2026
Mode: Standard