Rock Identifier
Diorite (Salt and Pepper Rock) (Diorite (comprising Plagioclase Feldspar, Hornblende, and Biotite)) — igneous
igneous

Diorite (Salt and Pepper Rock)

Diorite (comprising Plagioclase Feldspar, Hornblende, and Biotite)

Hardness: 6–7 Mohs. Color: Speckled black and white (salt and pepper). Luster: Dull to sub-vitreous. Texture: Phaneritic (coarse-grained). Cleavage: Two directions at nearly 90 degrees (in feldspar grains). Specific Gravity: 2.8–3.0.

Hardness
6–7 Mohs
Color
Speckled black and white (salt and pepper)
Luster
Dull to sub-vitreous
Identified More igneous

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Physical properties

Hardness: 6–7 Mohs. Color: Speckled black and white (salt and pepper). Luster: Dull to sub-vitreous. Texture: Phaneritic (coarse-grained). Cleavage: Two directions at nearly 90 degrees (in feldspar grains). Specific Gravity: 2.8–3.0.

Formation & geological history

Formed by the slow cooling of magma deep beneath the Earth's surface (intrusive/plutonic). Typically associated with volcanic arcs and subduction zones. This specific specimen has been further shaped by water erosion (river or beach pebble).

Uses & applications

Construction (crushed stone, base material), architectural stone (countertops, pavers), and historically used for carvings and sculptures due to its durability.

Geological facts

Diorite was used in ancient Egypt and Mesopotamia for sculptures; the famous Code of Hammurabi was inscribed on a massive basalt/diorite stele. It is often confused with Granite but contains little to no visible quartz.

Field identification & locations

Identify by its 'salt and pepper' appearance with crystals of roughly equal size. Unlike granite (which has pink/white/clear grains), diorite is strictly medium-to-dark grey and white. Commonly found in mountain ranges like the Andes or Cascade mountains.