Rock Identifier
Iron-stained quartz-rich rock (probable quartzite or silicified breccia) (Quartz-dominant aggregate, chiefly SiO₂, with iron oxides/hydroxides) — metamorphic
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 incorrect

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.

Identified More metamorphic
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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.