
metamorphic
Weathered quartz-rich rock, possibly quartzite
Quartzite (mostly SiO₂), with possible iron-oxide staining and minor feldspar or mica
AI-generated identification · may be incorrectHardness about 7 Mohs; gray-white to rusty brown, with a dull to glassy luster and granular, interlocking quartz texture. The irregular fracture and apparent lack of prominent cleavage are consistent with quartzite, though the image is insufficient for certainty.
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Physical properties
Hardness about 7 Mohs; gray-white to rusty brown, with a dull to glassy luster and granular, interlocking quartz texture. The irregular fracture and apparent lack of prominent cleavage are consistent with quartzite, though the image is insufficient for certainty.
Formation & geological history
Forms when quartz-rich sandstone is recrystallized during regional metamorphism, commonly during mountain-building events; its age depends on the original sandstone and metamorphic terrain.
Uses & applications
Used as crushed stone, aggregate, building stone, and decorative rock; attractive pieces may be collected but this specimen appears ordinary.
Geological facts
Iron oxides commonly produce the reddish-brown weathering colors. A steel knife should not scratch fresh quartz-rich surfaces, while quartzite typically scratches glass.
Field identification & locations
Common in metamorphic mountain belts worldwide, including the Appalachians, Rocky Mountains, Alps, and Scandinavian Shield. Confirm with a fresh surface, hardness test, and dilute-acid test; professional identification may distinguish it from weathered quartz or sandstone.
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