Rock Identifier
K-Feldspar (Potassium Feldspar (KAlSi3O8)) — mineral
mineral

K-Feldspar

Potassium Feldspar (KAlSi3O8)

AI-generated identification · may be incorrect

Hardness of 6 on the Mohs scale, pink to salmon-white color, vitreous to pearly luster, and distinct cleavage at nearly 90 degrees.

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Physical properties

Hardness of 6 on the Mohs scale, pink to salmon-white color, vitreous to pearly luster, and distinct cleavage at nearly 90 degrees.

Formation & geological history

Forms primarily in igneous rocks like granite and pegmatites through the slow cooling of silica-rich magma deep within the Earth's crust.

Uses & applications

Widely used in the manufacturing of ceramics, glass, porcelain, and occasionally as a minor decorative gemstone.

Geological facts

Feldspars are the single most abundant mineral group in the Earth's crust, making up about 60% of terrestrial rocks.

Field identification & locations

Easily identified in the field by its characteristic pink or salmon coloration and blocky crystal cleavage planes; found worldwide.