Rock Identifier
Feldspar (Aluminosilicate (KAlSi3O8 - NaAlSi3O8 - CaAl2Si2O8)) — mineral
mineral

Feldspar

Aluminosilicate (KAlSi3O8 - NaAlSi3O8 - CaAl2Si2O8)

AI-generated identification · may be incorrect

Hardness of 6 on the Mohs scale, typically white, gray, or pink in color with a vitreous to pearly luster and distinct cleavage planes at nearly 90 degrees.

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Physical properties

Hardness of 6 on the Mohs scale, typically white, gray, or pink in color with a vitreous to pearly luster and distinct cleavage planes at nearly 90 degrees.

Formation & geological history

Forms in igneous, metamorphic, and sedimentary rocks through the cooling of magma or crystallization from hydrothermal solutions.

Uses & applications

Widely used in the manufacture of ceramics, glass, porcelain, and as a flux in metallurgy.

Geological facts

Feldspar is the most abundant group of minerals in the Earth's crust, making up about 60% of terrestrial rocks.

Field identification & locations

Identified easily by its rectangular crystal habit, good cleavage, and hardness that scratches glass; found worldwide in granites and pegmatites.