Rock Identifier
Likely rough feldspar crystal (possibly amazonite or orthoclase) (Potassium feldspar, KAlSi₃O₈; exact variety cannot be confirmed from the image) — mineral
mineral

Likely rough feldspar crystal (possibly amazonite or orthoclase)

Potassium feldspar, KAlSi₃O₈; exact variety cannot be confirmed from the image

AI-generated identification · may be incorrect

Opaque, blocky crystal with salmon-brown and greenish areas and a dull to vitreous luster. Feldspar has Mohs hardness 6, two near-right-angle cleavage directions, and monoclinic or triclinic crystal structure depending on variety.

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Physical properties

Opaque, blocky crystal with salmon-brown and greenish areas and a dull to vitreous luster. Feldspar has Mohs hardness 6, two near-right-angle cleavage directions, and monoclinic or triclinic crystal structure depending on variety.

Formation & geological history

Crystallized from cooling, silica-rich magma, commonly in granites and pegmatites; potassium feldspar occurs in rocks spanning much of Earth’s geological history.

Uses & applications

Used in ceramics and glass; attractive, well-formed or colored crystals are collected and occasionally cut as gemstones.

Geological facts

Feldspar is the most abundant mineral group in Earth’s crust. The specimen’s color and crystal form are insufficient to identify a specific feldspar variety confidently.

Field identification & locations

Look for a blocky habit and two prominent cleavages meeting nearly at 90°; common sources include granites and pegmatites worldwide. A scratch test and fresh, clean surfaces can help distinguish feldspar from similar minerals.