
mineral
Quartz-rich rock, likely milky quartz or quartzite
Quartz (SiO₂), possibly in a quartzite or hydrothermal vein matrix
AI-generated identification · may be incorrectTranslucent gray-beige to pale brown, vitreous-to-waxy luster, irregular fracture, and no obvious cleavage; quartz hardness is Mohs 7, with specific gravity about 2.65. The granular, sparkly texture suggests intergrown quartz crystals, possibly with iron-oxide staining or minor feldspar/mica.
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Physical properties
Translucent gray-beige to pale brown, vitreous-to-waxy luster, irregular fracture, and no obvious cleavage; quartz hardness is Mohs 7, with specific gravity about 2.65. The granular, sparkly texture suggests intergrown quartz crystals, possibly with iron-oxide staining or minor feldspar/mica.
Formation & geological history
Likely formed when silica-rich fluids crystallized in a fracture, or when quartz-rich sandstone recrystallized during metamorphism. Exact age and origin cannot be determined from the photograph alone.
Uses & applications
Quartz is used in glass, ceramics, electronics, abrasives, and engineered stone; attractive pieces may be collected or cut for display, though this specimen appears more suitable as a cabinet specimen than jewelry material.
Geological facts
Quartz commonly shows conchoidal fracture and can scratch ordinary glass. Brown or golden coloration commonly results from iron oxides coating or staining the quartz.
Field identification & locations
Test with a steel knife and glass: quartz should resist the knife and scratch glass, though surface coatings can confuse results. Common sources include hydrothermal veins and quartzite terrains worldwide.
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