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

K-feldspar (Potassium Feldspar)

Microcline / Orthoclase (KAlSi3O8)

AI-generated identification · may be incorrect

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

Formation & geological history

Forms in igneous rocks like granite and pegmatites through slow cooling of magma rich in potassium and silica.

Uses & applications

Used in the manufacturing of ceramics, porcelain, glass, and occasionally as a minor gemstone or lapidary material.

Geological facts

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

Field identification & locations

Identify by its distinctive pink color, rectangular crystal habit, and two cleavage planes meeting at right angles.