Rock Identifier
K-feldspar (Potassium Feldspar (Orthoclase/Microcline, KAlSi3O8)) — mineral
mineral

K-feldspar

Potassium Feldspar (Orthoclase/Microcline, KAlSi3O8)

AI-generated identification · may be incorrect

Hardness of 6 on the Mohs scale, typically pink to reddish-brown in color, vitreous to pearly luster, and two directions of good cleavage at nearly 90 degrees.

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Physical properties

Hardness of 6 on the Mohs scale, typically pink to reddish-brown in color, vitreous to pearly luster, and two directions of good cleavage at nearly 90 degrees.

Formation & geological history

Forms primarily through the slow cooling of silica-rich felsic magmas like granite and pegmatite deep within the Earth's crust.

Uses & applications

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

Geological facts

It is one of the most abundant rock-forming minerals in the Earth's crust and is a primary component that gives many granites their distinct pinkish hue.

Field identification & locations

Identified easily by its characteristic salmon-pink color, blocky crystal habit, and rectangular cleavage angles; commonly found globally in continental granitic rocks.