
mineral
Milky quartz (likely quartz-rich rock)
Quartz, silicon dioxide (SiO₂)
AI-generated identification · may be incorrectWhite to translucent, vitreous-to-waxy luster, irregular fracture, and no obvious cleavage; Mohs hardness 7, with specific gravity about 2.65. The granular, cloudy appearance may indicate milky quartz or quartz in a weathered host rock.
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Physical properties
White to translucent, vitreous-to-waxy luster, irregular fracture, and no obvious cleavage; Mohs hardness 7, with specific gravity about 2.65. The granular, cloudy appearance may indicate milky quartz or quartz in a weathered host rock.
Formation & geological history
Forms when silica-rich fluids crystallize in veins, cavities, and fractures, or during cooling of granitic and metamorphic rocks. Quartz is abundant throughout geologic time; the specimen’s exact age cannot be determined visually.
Uses & applications
Common quartz is used in glass, ceramics, abrasives, engineered stone, and electronics; attractive pieces are collected or used decoratively. This rough specimen has modest commercial value.
Geological facts
Its cloudy appearance commonly results from microscopic fluid inclusions, fractures, or impurities. Quartz is one of Earth’s most abundant and chemically stable minerals.
Field identification & locations
Test with a steel file or quartz crystal: true quartz should resist scratching by steel, while it can scratch glass. Common worldwide in quartz veins, granite pegmatites, metamorphic rocks, and sedimentary gravels; the dark material may be iron/manganese staining or attached host rock.
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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