
mineral
Weathered quartz-rich rock, possibly milky quartz or quartz-bearing granite
Quartz (SiO₂), potentially with feldspar and iron-oxide staining
AI-generated identification · may be incorrectCream-white, opaque to translucent, with a dull to glassy luster and irregular fracture; quartz hardness is about 7 Mohs, with no cleavage. The image is insufficient to confirm crystal structure or specific gravity.
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Physical properties
Cream-white, opaque to translucent, with a dull to glassy luster and irregular fracture; quartz hardness is about 7 Mohs, with no cleavage. The image is insufficient to confirm crystal structure or specific gravity.
Formation & geological history
Likely formed by cooling of silica-rich magma or precipitation from hydrothermal fluids; its exact geological age and setting cannot be determined visually. Brown areas may be weathered iron oxides or attached host material.
Uses & applications
Common quartz is used in glass, ceramics, abrasives, electronics, and decorative stone; attractive pieces may be collected, but this specimen appears low-grade for jewelry.
Geological facts
Quartz commonly forms six-sided crystals, but massive quartz lacks obvious crystal faces. A steel knife should not scratch quartz, while quartz can scratch ordinary glass.
Field identification & locations
Look for glassy translucence, conchoidal fracture, and hardness; test on an inconspicuous area and avoid confusing it with calcite, which is softer and fizzes in dilute acid. Quartz-rich material occurs worldwide in veins, pegmatites, and igneous rocks.
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Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous