
metamorphic
Quartz-bearing metamorphic rock, likely quartzite
Quartzite; predominantly quartz (SiO₂), with possible feldspar, mica, and iron-oxide staining
AI-generated identification · may be incorrectWhite to gray, massive, sugary crystalline texture with rusty staining; vitreous to dull luster, no obvious cleavage, and likely Mohs hardness about 7. Quartzite is generally dense, tough, and scratches glass.
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Physical properties
White to gray, massive, sugary crystalline texture with rusty staining; vitreous to dull luster, no obvious cleavage, and likely Mohs hardness about 7. Quartzite is generally dense, tough, and scratches glass.
Formation & geological history
Formed when quartz-rich sandstone recrystallized under heat and pressure during regional metamorphism; its precise geological age cannot be determined from the image and depends on its source terrane.
Uses & applications
Used as crushed stone, aggregate, road material, building stone, and decorative slabs; attractive specimens may be collected, though this example appears common.
Geological facts
The dark gray rind may represent mica-rich schist, gneiss, or weathered host rock enclosing a quartz-rich vein or layer, so it could also be a quartz vein in metamorphic rock rather than pure quartzite.
Field identification & locations
Look for interlocking quartz grains, strong resistance to scratching, and lack of acid reaction; a glassy fracture and translucent edges support abundant quartz. Common in metamorphic mountain belts worldwide.
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