
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 incorrectOpaque, 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.
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