Rock Identifier
Rounded quartz-rich cobble, likely quartzite (Quartzite (mostly SiO₂); exact identification requires closer examination) — metamorphic
metamorphic

Rounded quartz-rich cobble, likely quartzite

Quartzite (mostly SiO₂); exact identification requires closer examination

AI-generated identification · may be incorrect

Tan to brown, granular, and rounded by abrasion; quartzite is typically Mohs 7, with a vitreous-to-dull luster and interlocking quartz grains. No obvious cleavage is visible.

Identified More metamorphic →
Explore Rounded quartz-rich cobble, likely quartzite in the encyclopedia →

Identify your own rocks.

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

Physical properties

Tan to brown, granular, and rounded by abrasion; quartzite is typically Mohs 7, with a vitreous-to-dull luster and interlocking quartz grains. No obvious cleavage is visible.

Formation & geological history

If quartzite, it formed when quartz-rich sandstone was metamorphosed and recrystallized under heat and pressure; its age cannot be determined from the image. The cobble was later rounded during transport by water or ice.

Uses & applications

Quartzite is used as crushed aggregate, paving and building stone, and occasionally as a decorative material; this cobble is mainly of modest collecting interest.

Geological facts

A useful clue for quartzite is that it tends to fracture through quartz grains rather than separating cleanly around them, unlike many sandstones.

Field identification & locations

The rounded shape suggests transport in a stream, shoreline, or glacial deposit. Similar quartz-rich cobbles occur widely; inspect a fresh break for fused, interlocking grains to distinguish quartzite from sandstone or other rocks.