
mineral
Quartz cluster, possibly druzy quartz on matrix
Quartz (SiO₂), likely microcrystalline to coarse crystalline; associated matrix uncertain
AI-generated identification · may be incorrectWhite to gray, sugary granular crystals with a vitreous to slightly dull luster; Mohs hardness 7, trigonal crystal structure, no cleavage, conchoidal fracture, specific gravity about 2.65. Exact identification is limited by the photograph.
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Physical properties
White to gray, sugary granular crystals with a vitreous to slightly dull luster; Mohs hardness 7, trigonal crystal structure, no cleavage, conchoidal fracture, specific gravity about 2.65. Exact identification is limited by the photograph.
Formation & geological history
Quartz commonly precipitates from silica-rich hydrothermal fluids in cavities, fractures, and veins, often coating older rock; formation may range from Precambrian to recent. The darker supporting material is likely weathered host rock or another mineral.
Uses & applications
Common quartz is used in glass, ceramics, abrasives, electronics, and engineered stone; attractive clusters are sold as display specimens. This piece has modest decorative and collecting value.
Geological facts
The granular surface may be druzy quartz, composed of many tiny quartz crystals. Quartz is one of Earth’s most abundant minerals and is resistant to chemical weathering.
Field identification & locations
Identify by its hardness, glassy sparkle, lack of cleavage, and inability to scratch it with a steel knife; a streak test should be white. Common sources include hydrothermal veins and geodes worldwide, especially Brazil, Morocco, and the United States.
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