
mineral
Quartz crystal cluster (likely druzy quartz)
Quartz, silicon dioxide (SiO₂)
AI-generated identification · may be incorrectWhite to pale gray, translucent crystals with a vitreous-to-sparkly luster; hardness 7 Mohs, trigonal crystal structure, no cleavage, and uneven to conchoidal fracture. The specimen appears to be quartz crystals on a light-colored matrix; exact minerals cannot be confirmed from the photo.
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Physical properties
White to pale gray, translucent crystals with a vitreous-to-sparkly luster; hardness 7 Mohs, trigonal crystal structure, no cleavage, and uneven to conchoidal fracture. The specimen appears to be quartz crystals on a light-colored matrix; exact minerals cannot be confirmed from the photo.
Formation & geological history
Quartz commonly crystallizes from silica-rich hydrothermal fluids in veins and cavities, or from groundwater in geodes. Its age depends on the host deposit and cannot be determined visually.
Uses & applications
Collected as a natural display specimen; quartz is also used in glassmaking, electronics, abrasives, and jewelry.
Geological facts
Druzy describes a surface covered with many small crystals rather than a distinct mineral species.
Field identification & locations
Look for hard, glassy crystals that scratch ordinary glass and resist scratching by a steel knife; quartz occurs worldwide in veins, geodes, and pegmatites. The photo does not show enough context to identify a specific locality or matrix.
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