Rock Identifier
Tumbled granite or granitic pebble (Granite; chiefly quartz, feldspar, and mica/amphibole) — igneous
igneous

Tumbled granite or granitic pebble

Granite; chiefly quartz, feldspar, and mica/amphibole

AI-generated identification · may be incorrect

Hardness about 6–7 Mohs; rounded and polished, mottled gray-brown with visible granular crystals and earthy iron staining; vitreous to dull luster, no obvious cleavage as a whole, specific gravity roughly 2.6–2.8.

Identified More igneous
Explore Tumbled granite or granitic pebble in the encyclopedia →

Identify your own rocks.

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

Physical properties

Hardness about 6–7 Mohs; rounded and polished, mottled gray-brown with visible granular crystals and earthy iron staining; vitreous to dull luster, no obvious cleavage as a whole, specific gravity roughly 2.6–2.8.

Formation & geological history

Slow cooling of silica-rich magma produced coarse interlocking crystals, typically during Precambrian to Phanerozoic continental crust formation; the photographed piece is naturally water-rounded or mechanically tumbled.

Uses & applications

Used as aggregate, building and paving stone, countertops, monuments, and landscaping rock; small tumbled pieces are inexpensive decor or teaching specimens.

Geological facts

Granite’s characteristic speckled appearance comes from contrasting light feldspar/quartz and dark mica or amphibole; surface staining can make it appear brown or greenish.

Field identification & locations

Identify it by its hard, granular texture and randomly interlocking light and dark minerals; common worldwide, especially in exposed continental shield and mountain regions. A definitive identification may require a fresh surface or hand lens.