Rock Identifier
Tumbled granite (Granite; chiefly quartz, alkali feldspar, plagioclase, and biotite/hornblende) — igneous
igneous

Tumbled granite

Granite; chiefly quartz, alkali feldspar, plagioclase, and biotite/hornblende

AI-generated identification · may be incorrect

Coarse-grained, speckled gray, cream, and black rock with a dull to slightly vitreous luster; hardness about 6–7 Mohs, no cleavage as a whole, and specific gravity roughly 2.63–2.75.

Identified More igneous
Explore Tumbled granite in the encyclopedia →

Identify your own rocks.

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

Physical properties

Coarse-grained, speckled gray, cream, and black rock with a dull to slightly vitreous luster; hardness about 6–7 Mohs, no cleavage as a whole, and specific gravity roughly 2.63–2.75.

Formation & geological history

An intrusive igneous rock crystallized slowly from silica-rich magma deep in Earth’s crust, commonly during Precambrian to Phanerozoic mountain-building events; this specimen has been rounded by tumbling.

Uses & applications

Used extensively for countertops, monuments, building stone, aggregate, and landscaping; polished pebbles are inexpensive decorative and educational specimens.

Geological facts

Visible interlocking grains distinguish granite from fine-grained volcanic rocks such as rhyolite. Black grains are typically biotite or amphibole, while translucent grains are quartz.

Field identification & locations

Identify it by its coarse interlocking texture and three-color speckling; it is common in continental shields, mountain belts, glacial deposits, and river gravels worldwide.