
mineral
Likely milky quartz
Quartz (silicon dioxide, SiO₂)
AI-generated identification · may be incorrectThe small, rough cream-white specimen appears opaque and irregular, with a vitreous-to-dull luster; quartz has Mohs hardness 7, a trigonal crystal structure, and no cleavage, breaking with a curved or uneven fracture. The photo does not show diagnostic crystal faces, so identification is tentative.
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Physical properties
The small, rough cream-white specimen appears opaque and irregular, with a vitreous-to-dull luster; quartz has Mohs hardness 7, a trigonal crystal structure, and no cleavage, breaking with a curved or uneven fracture. The photo does not show diagnostic crystal faces, so identification is tentative.
Formation & geological history
Quartz commonly forms when silica-rich fluids cool and crystallize in veins or fractures, and also occurs in many igneous and metamorphic rocks; it spans a vast range of geological ages.
Uses & applications
Quartz is used in glass, electronics, abrasives, and jewelry; attractive pieces may be collected or polished.
Geological facts
Quartz is one of Earth’s most abundant minerals and its hardness lets it scratch ordinary glass.
Field identification & locations
Look for glass-scratching hardness, lack of cleavage, and uneven fracture; quartz occurs worldwide, especially in veins and pegmatites. The specimen’s exact source cannot be determined from the image.
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