Rock Identifier
Red-orange feldspar crystal (likely orthoclase) (Potassium feldspar, KAlSi₃O₈ (likely orthoclase)) — mineral
mineral

Red-orange feldspar crystal (likely orthoclase)

Potassium feldspar, KAlSi₃O₈ (likely orthoclase)

AI-generated identification · may be incorrect

Opaque, salmon-red to orange, with a vitreous-to-dull luster and blocky shape; feldspar has Mohs hardness 6 and two near-90° cleavage directions. The photo does not show enough detail to confirm the species.

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Physical properties

Opaque, salmon-red to orange, with a vitreous-to-dull luster and blocky shape; feldspar has Mohs hardness 6 and two near-90° cleavage directions. The photo does not show enough detail to confirm the species.

Formation & geological history

Likely crystallized as part of an igneous rock, such as granite or pegmatite, as magma cooled; potassium feldspar is common in rocks spanning much of Earth’s geological history.

Uses & applications

Feldspar is used in glass and ceramic production; attractive crystals may be kept as inexpensive mineral specimens.

Geological facts

Red coloration commonly comes from tiny inclusions or staining rather than the feldspar itself.

Field identification & locations

Its blocky form and approximately right-angle cleavage are useful clues; distinguish it from quartz, which lacks cleavage. The image alone cannot establish locality or definitively identify the mineral.