Rock Identifier
Diorite (Plutonic Igneous Rock (Intermediate Composition)) — Igneous
Igneous

Diorite

Plutonic Igneous Rock (Intermediate Composition)

Hardness: 6-7 on Mohs scale. Color: Salt-and-pepper (mottled black and white). Luster: Phaneritic (coarse-grained) with sub-vitreous crystals. Crystal Structure: Monoclinic/Triclinic minerals; specific gravity: 2.8-3.0.

Hardness
6-7 on Mohs scale
Color
Salt-and-pepper (mottled black and white)
Luster
Phaneritic (coarse-grained) with sub-vitreous crystals
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale. Color: Salt-and-pepper (mottled black and white). Luster: Phaneritic (coarse-grained) with sub-vitreous crystals. Crystal Structure: Monoclinic/Triclinic minerals; 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 at subduction zones. Typically associated with mountain building through various geological eras.

Uses & applications

Used primarily as crushed stone for road construction and as a decorative stone for countertops, pavers, and building facades. Historically used in ancient Egypt and Mesopotamia for carving hard-stone sculptures.

Geological facts

Diorite was used to carve the Code of Hammurabi, one of the oldest deciphered writings of significant length in the world, due to the rock's extreme durability and hardness.

Field identification & locations

Identify in the field by its phaneritic texture with a roughly equal mix of light plagioclase feldspar and dark minerals like hornblende or biotite. It lacks the pinkish potassium feldspar found in granite and the higher concentration of quartz. Often found in batholiths and mountain ranges like the Andes.