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

Diorite

Diorite (Intermediate intrusive igneous rock)

Hardness: 6-7 on the Mohs scale. Color: Mottled 'salt and pepper' appearance (black and white). Luster: Phaneritic (crystalline). Crystal Structure: Coarse-grained phaneritic texture. Cleavage: Good in two directions via feldspar components. Specific Gravity: 2.8-3.0.

Hardness
6-7 on the Mohs scale
Color
Mottled 'salt and pepper' appearance (black and white)
Luster
Phaneritic (crystalline)
Identified More igneous

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Physical properties

Hardness: 6-7 on the Mohs scale. Color: Mottled 'salt and pepper' appearance (black and white). Luster: Phaneritic (crystalline). Crystal Structure: Coarse-grained phaneritic texture. Cleavage: Good in two directions via feldspar components. Specific Gravity: 2.8-3.0.

Formation & geological history

Formed from the slow cooling of magma beneath the Earth's surface in volcanic arcs and mountain-building zones (subduction zones). It is typically of Phanerozoic age but can be found in older Precambrian shields.

Uses & applications

Commonly used as a base material in construction, crushed stone for roads, and occasionally as a polished 'granite' for countertops and floor tiles. Historically used by ancient civilizations for sculpture and tools due to its extreme hardness.

Geological facts

The Code of Hammurabi, one of the oldest deciphered writings of significant length in the world, was inscribed on a 7-foot tall stele made of polished black diorite. It is often confused with granite but lacks significant quartz content.

Field identification & locations

Identify in the field by its distinctive 'salt and pepper' look where the light (plagioclase feldspar) and dark (hornblende or biotite) minerals are roughly equal. Found in large mountain ranges like the Andes or the Cascades. Collectors look for pieces with large, well-defined amphibole crystals.