Rock Identifier
Quartz-rich mineral specimen, possibly druzy quartz (Quartz (SiO₂), possibly with carbonate or feldspar matrix) — mineral
mineral

Quartz-rich mineral specimen, possibly druzy quartz

Quartz (SiO₂), possibly with carbonate or feldspar matrix

AI-generated identification · may be incorrect

Pale cream to gray, translucent granular crystals with a vitreous to slightly pearly luster; likely Mohs hardness about 7 for quartz, with irregular fracture and no obvious cleavage. The small size and matrix make exact identification uncertain from the image alone.

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Physical properties

Pale cream to gray, translucent granular crystals with a vitreous to slightly pearly luster; likely Mohs hardness about 7 for quartz, with irregular fracture and no obvious cleavage. The small size and matrix make exact identification uncertain from the image alone.

Formation & geological history

Likely formed when silica-rich fluids deposited quartz crystals in a cavity, vein, or weathered host rock; age depends on its geological setting and cannot be determined visually.

Uses & applications

Common quartz is used in glass, ceramics, abrasives, electronics, and construction; attractive crystal clusters are collected or used decoratively. This specimen appears more suitable for a small collection than jewelry.

Geological facts

The bright granular surfaces resemble druzy quartz, though similar appearances can result from calcite or weathered feldspar. A hardness test, streak, acid reaction, and magnification would improve identification.

Field identification & locations

Look for glassy luster, six-sided crystal faces, and inability to scratch quartz with a steel knife; quartz should scratch glass. Common sources include hydrothermal veins and cavities worldwide, especially Brazil, Mexico, the United States, and Madagascar.