
metamorphic
Weathered quartz-rich cobble, likely quartzite
Quartzite (mostly microcrystalline SiO₂), possibly quartz-rich sandstone or vein quartz
AI-generated identification · may be incorrectHardness about 7 Mohs; opaque cream, honey-yellow to brown surface with white quartz patches, vitreous to dull luster, massive granular texture, and no obvious cleavage. The yellow-brown coloration likely comes from iron-oxide staining and weathering.
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Physical properties
Hardness about 7 Mohs; opaque cream, honey-yellow to brown surface with white quartz patches, vitreous to dull luster, massive granular texture, and no obvious cleavage. The yellow-brown coloration likely comes from iron-oxide staining and weathering.
Formation & geological history
Quartzite forms when quartz sandstone is recrystallized under heat and pressure during metamorphism; the specimen’s exact age and source cannot be determined from the image. It may also be weathered vein quartz or silicified sandstone.
Uses & applications
Used as crushed stone, aggregate, road material, building stone, and decorative rock; attractive pieces may be tumbled or collected. This ordinary cobble has minimal commercial value.
Geological facts
Quartzite commonly preserves interlocking quartz grains and breaks across grains rather than around them, producing a very hard, durable surface.
Field identification & locations
Common in metamorphic terrains and river gravels worldwide, including the Appalachians, Rocky Mountains, and many shield regions. A steel nail should not scratch it; acid typically produces no reaction, helping distinguish it from limestone.
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