Rock Identifier
Diorite (Intermediate plutonic igneous rock) — igneous
igneous

Diorite

Intermediate plutonic igneous rock

Hardness: 6-7 on Mohs scale. Color: Salt-and-pepper appearance due to a mix of light plagioclase feldspar and dark minerals like hornblende and biotite. Luster: Vitreous to dull. Crystal structure: Phaneritic (coarse-grained). Specific gravity: 2.8-3.0.

Hardness
6-7 on Mohs scale
Luster
Vitreous to dull
Identified More igneous
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Physical properties

Hardness: 6-7 on Mohs scale. Color: Salt-and-pepper appearance due to a mix of light plagioclase feldspar and dark minerals like hornblende and biotite. Luster: Vitreous to dull. Crystal structure: Phaneritic (coarse-grained). Specific gravity: 2.8-3.0.

Formation & geological history

Formed from the slow cooling of magma beneath the Earth's surface, typically containing intermediate amounts of silica. Common in subduction zone settings, often associated with continental volcanic arcs.

Uses & applications

Used widely in construction and architecture as crushed stone, dimension stone, and decorative aggregate. Historically used for ancient carvings such as the Code of Hammurabi.

Geological facts

Diorite is extremely hard and tough to work with, which is why ancient civilizations prized it for monuments. It is compositionally intermediate between granite and gabbro.

Field identification & locations

Easily identified in the field by its distinct salt-and-pepper texture lacking the significant quartz content of granite. Commonly found in mountain belts worldwide.