
metamorphic
Weathered quartz-rich stone, possibly quartzite
Quartzite (mostly SiO₂), possibly quartz-bearing sandstone or granite fragment
AI-generated identification · may be incorrectHardness about 7 Mohs; brown, gray, and white mottling; vitreous to dull luster; massive, granular texture with no obvious cleavage. White areas likely quartz, while brown coloration may reflect iron-oxide staining or weathering.
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Physical properties
Hardness about 7 Mohs; brown, gray, and white mottling; vitreous to dull luster; massive, granular texture with no obvious cleavage. White areas likely quartz, while brown coloration may reflect iron-oxide staining or weathering.
Formation & geological history
If quartzite, it formed when quartz-rich sandstone was recrystallized under metamorphic heat and pressure, commonly during mountain building. The image alone cannot establish its geological age or distinguish it confidently from weathered quartz-bearing igneous rock.
Uses & applications
Quartzite is used as crushed aggregate, roadstone, building stone, countertops, and decorative material; attractive pieces may be collected but this specimen appears ordinary.
Geological facts
Quartzite commonly fractures across grains rather than splitting along bedding, and its quartz content makes it resistant to scratching by steel. Iron oxides often produce rusty brown surfaces and patches.
Field identification & locations
Test with a steel knife: genuine quartz-rich material should resist scratching; glass can help test hardness if available. Common sources include mountain belts and ancient sandstone terrains worldwide.
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