
mineral
Quartz cluster
Quartz (silicon dioxide, SiO₂), likely milky quartz
AI-generated identification · may be incorrectWhite to translucent, vitreous-to-pearly luster, irregular intergrown crystals, and no obvious cleavage; Mohs hardness 7, trigonal crystal system, specific gravity about 2.65.
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Physical properties
White to translucent, vitreous-to-pearly luster, irregular intergrown crystals, and no obvious cleavage; Mohs hardness 7, trigonal crystal system, specific gravity about 2.65.
Formation & geological history
Forms when silica-rich fluids cool in cavities, veins, or fractures, commonly in igneous and metamorphic rocks. The specimen’s exact geological age and locality cannot be determined from the image.
Uses & applications
Used for ornamental specimens, lapidary work, glass, ceramics, electronics, and industrial abrasives; this small cluster has modest decorative and collecting value.
Geological facts
Milky appearance results from microscopic fluid inclusions, fractures, or impurities that scatter light. Quartz is one of Earth’s most abundant and chemically durable minerals.
Field identification & locations
Identify it by its glassy luster, hardness sufficient to scratch ordinary glass, lack of cleavage, and six-sided prismatic crystal habit when developed. Common sources include Brazil, Madagascar, the United States, and China.
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