Rock Identifier
Quartz-rich pegmatite, possibly milky quartz with muscovite (Quartz (SiO₂) with probable muscovite mica [KAl₂(AlSi₃O₁₀)(OH)₂]) — igneous
igneous

Quartz-rich pegmatite, possibly milky quartz with muscovite

Quartz (SiO₂) with probable muscovite mica [KAl₂(AlSi₃O₁₀)(OH)₂]

AI-generated identification · may be incorrect

Hardness about 2–2.5 for muscovite and 7 for quartz; pale gray-white, vitreous to pearly luster, irregular granular crystals, and prominent mica cleavage. The specimen appears coarse-grained and sparkly, though exact identification is limited by the photograph.

Identified More igneous
Explore Quartz-rich pegmatite, possibly milky quartz with muscovite in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness about 2–2.5 for muscovite and 7 for quartz; pale gray-white, vitreous to pearly luster, irregular granular crystals, and prominent mica cleavage. The specimen appears coarse-grained and sparkly, though exact identification is limited by the photograph.

Formation & geological history

Likely formed as a slowly cooled, silica-rich granitic pegmatite melt, allowing large quartz and mica crystals to grow; commonly Precambrian to Phanerozoic in age. It may also be a quartz-mica vein fragment.

Uses & applications

Quartz pegmatite is used for silica, ceramics, glass, and construction aggregate; attractive pieces are collected as mineral specimens. Muscovite has historical electrical and industrial uses, while gem-quality quartz may be cut or polished.

Geological facts

The reflective flakes are characteristic of mica, whose sheets separate into thin elastic layers; quartz is much harder and will scratch ordinary glass.

Field identification & locations

Look for glassy gray-white quartz intergrown with silvery, sheet-like mica and uneven fracture. Common in granitic terrains and pegmatite districts worldwide, including Brazil, the United States, India, and Madagascar.