Rock Identifier
Quartz-rich pegmatite (likely milky quartz with mica) (Quartz (SiO₂), with possible muscovite/biotite mica; exact rock identification is uncertain from the photo) — igneous
igneous

Quartz-rich pegmatite (likely milky quartz with mica)

Quartz (SiO₂), with possible muscovite/biotite mica; exact rock identification is uncertain from the photo

AI-generated identification · may be incorrect

Coarse, pale gray-white, irregularly crystalline and sparkly. Quartz has Mohs hardness 7, vitreous luster, and a hexagonal crystal structure; mica flakes are softer and split into sheets.

Identified More igneous →
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Physical properties

Coarse, pale gray-white, irregularly crystalline and sparkly. Quartz has Mohs hardness 7, vitreous luster, and a hexagonal crystal structure; mica flakes are softer and split into sheets.

Formation & geological history

Likely formed as a coarse-grained igneous pegmatite from slowly cooling, silica-rich residual magma, often in veins within older rocks. Its age cannot be determined from appearance alone.

Uses & applications

Quartz-rich material is used for glass, silica products, and decorative stone; mica is used in electrical and industrial products. This rough specimen appears to have modest decorative or collecting value.

Geological facts

Pegmatites can contain exceptionally large crystals and concentrated rare minerals, though none are clearly identifiable here.

Field identification & locations

Look for interlocking, coarse crystals and glittering mica flakes; quartz should scratch glass and resist a steel knife. Pegmatites occur worldwide, commonly near granite intrusions.