Rock Identifier
Milky quartz crystal fragment (Quartz, silicon dioxide (SiO₂)) — mineral
mineral

Milky quartz crystal fragment

Quartz, silicon dioxide (SiO₂)

AI-generated identification · may be incorrect

Hardness 7 Mohs; translucent white to colorless with a vitreous luster and conchoidal fracture. Trigonal crystal structure; no cleavage. The brown spots appear to be iron-oxide staining or inclusions.

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Physical properties

Hardness 7 Mohs; translucent white to colorless with a vitreous luster and conchoidal fracture. Trigonal crystal structure; no cleavage. The brown spots appear to be iron-oxide staining or inclusions.

Formation & geological history

Forms when silica-rich fluids crystallize in veins, cavities, or pegmatites; quartz occurs in rocks of many ages. The specimen’s exact age and source cannot be determined from the image.

Uses & applications

Quartz is used in glassmaking, electronics, abrasives, and decorative objects; attractive crystals are collected or used in jewelry.

Geological facts

Quartz is one of Earth’s most abundant minerals and is highly resistant to weathering.

Field identification & locations

Look for glassy translucence, hardness sufficient to scratch glass, and lack of cleavage; common worldwide in veins and many rock types. This small, irregular fragment has limited collector value.