Rock Identifier
Dark granite or granitic gneiss (Granite; quartz + feldspar + biotite/hornblende, possibly weakly gneissic) — igneous
igneous

Dark granite or granitic gneiss

Granite; quartz + feldspar + biotite/hornblende, possibly weakly gneissic

AI-generated identification · may be incorrect

Coarse-grained, dark gray to black with pale crystals and mottled texture; vitreous quartz and blocky feldspar are likely. Hardness is about 6–7 Mohs, with no obvious cleavage as a whole rock and high durability; exact identification is limited by the photograph.

Identified More igneous
Explore Dark granite or granitic gneiss in the encyclopedia →

Identify your own rocks.

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

Physical properties

Coarse-grained, dark gray to black with pale crystals and mottled texture; vitreous quartz and blocky feldspar are likely. Hardness is about 6–7 Mohs, with no obvious cleavage as a whole rock and high durability; exact identification is limited by the photograph.

Formation & geological history

Likely crystallized slowly from silica-rich magma deep in the crust, generally during Precambrian to Phanerozoic mountain-building events; if foliated, it may be metamorphosed granitic gneiss. Commonly forms plutons, batholiths, and exposed basement terrains.

Uses & applications

Used as dimension stone, paving, curbing, aggregate, monuments, countertops, and landscaping rock; attractive polished pieces may be used decoratively but this specimen is not typically gem-grade.

Geological facts

The pale patches may be feldspar and quartz, while dark areas are biotite or amphibole; weathering can produce the rough, speckled surface visible here. A fresh broken surface and a hand lens would distinguish granite from basalt or gneiss more reliably.

Field identification & locations

Common worldwide, including the United States, Canada, Scandinavia, India, and Brazil. Look for interlocking visible crystals; alignment or banding suggests gneiss, whereas uniformly crystalline texture favors granite.