Rock Identifier
Tumbled granite (likely black granite) (Granite; predominantly quartz (SiO₂), feldspar, and biotite/hornblende) — igneous
igneous

Tumbled granite (likely black granite)

Granite; predominantly quartz (SiO₂), feldspar, and biotite/hornblende

AI-generated identification · may be incorrect

Coarse, interlocking crystalline texture with black, white, and pink-brown grains; typically Mohs 6–7, vitreous to dull luster, no regular cleavage as a whole, and specific gravity about 2.6–2.8.

Identified More igneous
Explore Tumbled granite (likely black granite) in the encyclopedia →

Identify your own rocks.

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

Physical properties

Coarse, interlocking crystalline texture with black, white, and pink-brown grains; typically Mohs 6–7, vitreous to dull luster, no regular cleavage as a whole, and specific gravity about 2.6–2.8.

Formation & geological history

An intrusive igneous rock crystallized slowly from silica-rich magma deep in Earth’s crust, generally during Precambrian or younger continental plutonic events; this piece has been rounded by tumbling.

Uses & applications

Used for countertops, monuments, building stone, aggregate, landscaping, and inexpensive decorative specimens; generally low jewelry value.

Geological facts

The dark grains are commonly biotite or amphibole, while light grains are feldspar and quartz; the visible grain size indicates slow underground cooling.

Field identification & locations

Identify it by its speckled, interlocking grains and inability to scratch glass easily; common worldwide, especially in continental shields and mountain plutons.