
metamorphic
Weathered quartz-bearing rock, possibly iron-stained quartzite
Quartzite (mostly SiO₂), tentatively identified
AI-generated identification · may be incorrectBrown to tan, irregular and fine-grained with white granular patches likely quartz; dull to weakly glassy luster. Quartz hardness is about Mohs 7, with no obvious cleavage; exact texture and density are difficult to determine from the image.
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Physical properties
Brown to tan, irregular and fine-grained with white granular patches likely quartz; dull to weakly glassy luster. Quartz hardness is about Mohs 7, with no obvious cleavage; exact texture and density are difficult to determine from the image.
Formation & geological history
Likely formed when quartz-rich sandstone was metamorphosed and recrystallized, with brown coloration caused by iron-oxide weathering. Its geological age cannot be determined visually; quartzite occurs in rocks ranging from Precambrian to modern metamorphic belts.
Uses & applications
Common quartzite is used as crushed stone, aggregate, building stone, and decorative landscaping material; this small specimen has minimal commercial or jewelry value.
Geological facts
The white areas may be quartz veins or unweathered quartz grains, while the rusty-brown color commonly reflects hematite or limonite. A steel file should not scratch fresh quartz-rich surfaces.
Field identification & locations
Common in metamorphic mountain belts and stream gravels worldwide, especially where quartz-rich sandstone is exposed. Confirm with a hardness test, streak test, and close inspection for fused quartz grains; it could also be weathered quartz-rich sedimentary rock.
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