Rock Identifier
Diorite (Diorite, a coarse-grained intermediate intrusive igneous rock composed mainly of plagioclase feldspar and hornblende, with minor biotite, pyroxene, and quartz.) — igneous
igneous

Diorite

Diorite, a coarse-grained intermediate intrusive igneous rock composed mainly of plagioclase feldspar and hornblende, with minor biotite, pyroxene, and quartz.

AI-generated identification · may be incorrect

Typically dark gray-green with a salt-and-pepper texture, granular luster, and interlocking crystals; Mohs hardness is about 6–7, with no prominent cleavage as a rock and specific gravity around 2.7–2.9.

Identified More igneous
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Physical properties

Typically dark gray-green with a salt-and-pepper texture, granular luster, and interlocking crystals; Mohs hardness is about 6–7, with no prominent cleavage as a rock and specific gravity around 2.7–2.9.

Formation & geological history

Forms when intermediate-composition magma cools slowly underground, producing visible crystals; specimens may range from Precambrian to much younger ages. The image is consistent with diorite, though precise identification requires fresh surface and mineral testing.

Uses & applications

Used as crushed aggregate, road stone, dimension stone, paving, and occasionally countertops or monuments; it has limited gemstone value.

Geological facts

Diorite lies compositionally between granite and gabbro and commonly displays a distinctive black-and-white or greenish salt-and-pepper appearance.

Field identification & locations

Common in continental plutons, volcanic-arc batholiths, and mountain belts worldwide. Identify it by its coarse interlocking grains, abundant pale plagioclase, and dark amphibole/biotite; unlike granite, it has little visible quartz or pink feldspar.