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

Diorite

Diorite (Intermediate intrusive igneous rock)

Hardness: 6-7 on Mohs scale; Color: 'Salt and pepper' (mottled black and white); Luster: Phaneritic (crystalline/dull to vitreous); Crystal Structure: Coarse-grained intrusive; Cleavage: Good in two directions (due to feldspar and amphibole); Specific Gravity: 2.8 - 3.0

Hardness
6-7 on Mohs scale
Color
'Salt and pepper' (mottled black and white)
Luster
Phaneritic (crystalline/dull to vitreous)
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 (crystalline/dull to vitreous); Crystal Structure: Coarse-grained intrusive; Cleavage: Good in two directions (due to feldspar and amphibole); Specific Gravity: 2.8 - 3.0

Formation & geological history

Formed by the slow cooling of magma beneath the Earth's surface in volcanic arches and subduction zones. It has a chemical composition intermediate between granite and gabbro. Most specimens range from Precambrian to Cenozoic in age.

Uses & applications

Used in construction as crushed stone or road base. It is also polished for use as dimension stone for countertops, floor tiles, and building veneers. In ancient times, it was used by Egyptians and Sumerians for monumental sculpture due to its extreme hardness.

Geological facts

Diorite was used by the ancient Mesopotamians to carve the famous 'Code of Hammurabi' (stela), now in the Louvre. Its durability is so high that it is often difficult to carve without modern tools.

Field identification & locations

Identify in the field by its distinctive black-and-white 'dalmatian' appearance. It contains mostly white plagioclase feldspar and dark minerals like hornblende or biotite. It lacks the pinkish potassium feldspar and high quartz content found in granite. Found commonly in the Andes Mountains, Italy, and the UK.