Rock Identifier
Quartz-rich metamorphic rock, likely quartzite (Quartzite; predominantly crystalline quartz (SiO₂), possibly with mica, feldspar, and iron-oxide staining) — metamorphic
metamorphic

Quartz-rich metamorphic rock, likely quartzite

Quartzite; predominantly crystalline quartz (SiO₂), possibly with mica, feldspar, and iron-oxide staining

AI-generated identification · may be incorrect

Hardness about 7 Mohs; pale gray, cream, and tan with brown weathering; vitreous to dull luster and granular, interlocking quartz crystals. Typically lacks cleavage, breaks irregularly, and has specific gravity near 2.65;…

Identified More metamorphic
Explore Quartz-rich metamorphic rock, likely quartzite in the encyclopedia →

Identify your own rocks.

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

Physical properties

Hardness about 7 Mohs; pale gray, cream, and tan with brown weathering; vitreous to dull luster and granular, interlocking quartz crystals. Typically lacks cleavage, breaks irregularly, and has specific gravity near 2.65; the visible layered texture could also indicate quartz-rich schist or strongly metamorphosed sandstone.

Formation & geological history

Forms when quartz-rich sandstone is recrystallized under heat and pressure during mountain-building; individual specimens commonly range from Precambrian to Paleozoic age depending on locality. Exact identification and age require a fresh surface and locality information.

Uses & applications

Durable quartzite is used as crushed stone, aggregate, building stone, paving, and countertops; attractive pieces are collected but this rough specimen has little gem value.

Geological facts

A steel file should barely scratch it, while quartzite can scratch ordinary glass. Acid typically produces no fizz unless carbonate minerals are present.

Field identification & locations

Look for fused quartz grains, high hardness, and resistance to weathering; a sugary granular texture supports quartzite, whereas obvious aligned mica flakes suggest quartz-mica schist. Common in metamorphic mountain belts worldwide.