
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 incorrectCoarse, 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.