Rock Identifier
Iron-stained quartzite (likely) (Quartz-rich quartzite, predominantly SiO₂, with iron-oxide staining) — metamorphic
metamorphic

Iron-stained quartzite (likely)

Quartz-rich quartzite, predominantly SiO₂, with iron-oxide staining

AI-generated identification · may be incorrect

Massive, coarse-grained, mostly tan to cream with rusty red-brown patches; vitreous to dull luster. Quartz hardness is 7 Mohs; individual grains are interlocked, with no obvious cleavage. The image alone cannot confirm the identification or specific gravity.

Identified More metamorphic →
Explore Iron-stained quartzite (likely) in the encyclopedia →

Identify your own rocks.

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

Physical properties

Massive, coarse-grained, mostly tan to cream with rusty red-brown patches; vitreous to dull luster. Quartz hardness is 7 Mohs; individual grains are interlocked, with no obvious cleavage. The image alone cannot confirm the identification or specific gravity.

Formation & geological history

Quartz-rich sandstone recrystallized under heat and pressure into quartzite; iron oxides can produce the colored patches. Such rocks form in many geologic eras, so age cannot be determined from the photograph.

Uses & applications

Quartzite is used as dimension stone, aggregate, and decorative landscaping stone; this rounded specimen is mainly suitable for collecting or display.

Geological facts

Quartzite is tougher than ordinary sandstone because recrystallized quartz grains are tightly intergrown.

Field identification & locations

The rounded, weathered shape and quartz-rich appearance fit a natural rock specimen, but a close inspection of grain boundaries or a hardness test would help distinguish quartzite from quartz-rich vein rock. Quartzite occurs worldwide, especially in mountain belts.