Rock Identifier
Polished granitic pebble (Granite, composed chiefly of quartz, feldspar, and mica/amphibole) — igneous
igneous

Polished granitic pebble

Granite, composed chiefly of quartz, feldspar, and mica/amphibole

AI-generated identification · may be incorrect

Coarse, mottled white, gray, black, and brown grains with vitreous to dull luster; interlocking crystals, no obvious cleavage as a whole, Mohs hardness about 6–7, and specific gravity around 2.6–2.8.

Identified More igneous
Explore Polished granitic pebble in the encyclopedia →

Identify your own rocks.

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

Physical properties

Coarse, mottled white, gray, black, and brown grains with vitreous to dull luster; interlocking crystals, no obvious cleavage as a whole, Mohs hardness about 6–7, and specific gravity around 2.6–2.8.

Formation & geological history

A felsic intrusive igneous rock formed by slow cooling of silica-rich magma deep in Earth’s crust, commonly during Precambrian to Phanerozoic mountain-building events; the rounded shape is likely from stream or glacial abrasion and polishing.

Uses & applications

Used extensively for countertops, monuments, paving, building stone, aggregate, and landscaping; this small polished piece is mainly decorative or suitable for a teaching/collection specimen.

Geological facts

The brown areas may be iron-oxide staining or weathered feldspar, while dark patches likely contain biotite, hornblende, or mafic inclusions.

Field identification & locations

Identify it by visible interlocking light quartz/feldspar and dark mica or amphibole grains, unlike sedimentary rocks’ layers or metamorphic foliation; common worldwide, especially in continental shields and mountain belts.