Rock Identifier
Rounded quartz-rich pebble, possibly quartzite or granitic gneiss (Quartzite (mostly SiO₂) or quartz-rich granitoid; exact identification requires testing) — metamorphic
metamorphic

Rounded quartz-rich pebble, possibly quartzite or granitic gneiss

Quartzite (mostly SiO₂) or quartz-rich granitoid; exact identification requires testing

AI-generated identification · may be incorrect

Gray-white, fine- to medium-grained, dull to slightly glassy luster, rounded by abrasion; quartz hardness is 7 Mohs, with no obvious cleavage. The rusty-brown surface may be iron-oxide staining or weathered feldspar/mica.

Identified More metamorphic
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Physical properties

Gray-white, fine- to medium-grained, dull to slightly glassy luster, rounded by abrasion; quartz hardness is 7 Mohs, with no obvious cleavage. The rusty-brown surface may be iron-oxide staining or weathered feldspar/mica.

Formation & geological history

Likely a glacially or stream-transported pebble eroded from quartzite, granite, or gneiss; its rounded shape reflects prolonged abrasion. The original rock may be Precambrian or younger, but age cannot be determined visually.

Uses & applications

Suitable mainly as a decorative stone, landscaping pebble, or teaching specimen; not gem-grade and unlikely to have commercial construction value as a single pebble.

Geological facts

Quartzite commonly resists weathering and accumulates in gravel beds, beaches, and glacial deposits. A streak test, hardness test, and inspection of fresh surfaces would distinguish it from granite or gneiss.

Field identification & locations

Common in gravel and shoreline deposits worldwide; scratch testing with a steel knife (quartz should resist) and examining grain boundaries with a loupe are useful field methods. Effervescence with dilute acid would suggest carbonate rock instead.