Rock Identifier
Weathered quartz-rich rock, possibly milky quartz or quartz-bearing granite (Quartz (SiO₂), potentially with feldspar and iron-oxide staining) — mineral
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 incorrect

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.

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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.