Rock Identifier
Diorite (Phaneritic Intermediate Igneous Rock) — igneous
igneous

Diorite

Phaneritic Intermediate Igneous Rock

Hardness: 6-7 Mohs; Color: Salt-and-pepper (white and black/dark gray); Luster: Dull to sub-vitreous; Crystal Structure: Phaneritic (coarse-grained coarse crystals visible to the eye); Cleavage: Good in two directions (due to feldspar and amphibole); Specific Gravity: 2.8-3.0.

Hardness
6-7 Mohs
Color
Salt-and-pepper (white and black/dark gray)
Luster
Dull to sub-vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 Mohs; Color: Salt-and-pepper (white and black/dark gray); Luster: Dull to sub-vitreous; Crystal Structure: Phaneritic (coarse-grained coarse crystals visible to the eye); Cleavage: Good in two directions (due to feldspar and amphibole); Specific Gravity: 2.8-3.0.

Formation & geological history

Formed through the slow cooling of magma beneath the Earth's surface in volcanic arcs and mountain-building zones (subduction zones). It is typically of Precambrian to Cenozoic age.

Uses & applications

Used primarily as a crushed stone for construction base, road building, and drainage. High-quality specimens are used as 'black granite' for countertops, floor tiles, and ornamental stonework (sculptures).

Geological facts

In antiquity, diorite was highly prized for its extreme hardness. The Code of Hammurabi was inscribed on a massive stele of black diorite. It is often referred to as 'salt-and-pepper rock' because of its speckled appearance.

Field identification & locations

Identify by its coarse-grained texture and roughly equal balance of light and dark minerals. Common in batholiths and mountain ranges like the Andes. Collectors look for even distribution of minerals and lack of weathering.