
metamorphic
Iron-stained quartz-rich rock (probable quartzite or silicified breccia)
Quartz-dominant aggregate, chiefly SiO₂, with iron oxides/hydroxides
AI-generated identification · may be incorrectHardness about 7; brown, cream, gray, and rusty red, with a glassy to dull luster and irregular granular/vein-like texture. Quartz lacks cleavage and shows uneven fracture; iron staining produces the brown coloration.
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Physical properties
Hardness about 7; brown, cream, gray, and rusty red, with a glassy to dull luster and irregular granular/vein-like texture. Quartz lacks cleavage and shows uneven fracture; iron staining produces the brown coloration.
Formation & geological history
Likely formed when quartz-rich sediment or fractured rock was cemented and/or metamorphosed, then weathered and oxidized by groundwater. Exact age and locality cannot be determined from the photograph.
Uses & applications
Primarily a collector or teaching specimen; quartzite may be used as crushed stone, aggregate, or building stone, though this small irregular piece has negligible industrial value.
Geological facts
The metallic-looking highlights are probably reflective quartz faces or iron-oxide coatings rather than native metal. A steel file should not easily scratch fresh quartz surfaces.
Field identification & locations
Common in metamorphic terrains, hydrothermal veins, and weathered iron-rich zones worldwide; test with a hand lens, streak plate, and hardness test, while avoiding damage to potentially valuable surfaces.
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