
metamorphic
Quartz-rich metamorphic rock, likely quartzite
Quartzite; predominantly microcrystalline quartz (SiO₂), with possible iron-oxide staining and minor mica/feldspar
AI-generated identification · may be incorrectHardness about 7 Mohs; mottled gray, tan, orange, and rusty brown; vitreous to dull luster; interlocking granular texture, massive structure, and no obvious cleavage. The orange coloration likely reflects hematite or limonite.
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Physical properties
Hardness about 7 Mohs; mottled gray, tan, orange, and rusty brown; vitreous to dull luster; interlocking granular texture, massive structure, and no obvious cleavage. The orange coloration likely reflects hematite or limonite.
Formation & geological history
Formed when quartz-rich sandstone was deeply buried and recrystallized under heat and pressure, commonly during Precambrian or Paleozoic mountain-building. Exact age cannot be determined from the image.
Uses & applications
Used as crushed stone, aggregate, road material, building stone, and decorative landscape rock; attractive pieces may be polished or collected. This specimen has modest commercial value unless provenance or exceptional patterning is established.
Geological facts
Quartzite commonly preserves original bedding faintly but breaks across grains rather than around them, producing very hard, resistant boulders. Iron staining can create vivid breccia-like orange and red patterns.
Field identification & locations
Likely quartzite if it scratches glass and shows a sugary quartz texture; unlike sandstone, it should not crumble along grains. Common in metamorphic mountain belts and glacial or stream gravels.
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