Rock Identifier
Likely milky quartz (Quartz (silicon dioxide, SiO₂)) — mineral
mineral

Likely milky quartz

Quartz (silicon dioxide, SiO₂)

AI-generated identification · may be incorrect

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.

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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.