Rock Identifier
Granodiorite (Phaneritic Plutonic Rock (Intermediate)) — igneous
igneous

Granodiorite

Phaneritic Plutonic Rock (Intermediate)

Hardness: 6-7 on Mohs scale; Color: Salt and pepper (mottled grey/white/black); Luster: Vitreous to dull; Crystal structure: Phaneritic (medium to coarse-grained); Specific gravity: 2.6-2.7

Hardness
6-7 on Mohs scale
Color
Salt and pepper (mottled grey/white/black)
Luster
Vitreous to dull
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale; Color: Salt and pepper (mottled grey/white/black); Luster: Vitreous to dull; Crystal structure: Phaneritic (medium to coarse-grained); Specific gravity: 2.6-2.7

Formation & geological history

Formed through the slow crystallization of magma beneath the Earth's surface. It is typical of continental crust and often forms in volcanic arcs and mountain-building regions over millions of years.

Uses & applications

Used widely in heavy construction, road building, as crushed stone, and as a polished dimension stone for countertops and architectural cladding.

Geological facts

Granodiorite is the rock type that makes up the famous Rosetta Stone. It is chemically intermediate between granite and diorite, containing more plagioclase feldspar than orthoclase.

Field identification & locations

Identify by looking for a speckled 'salt and pepper' appearance with crystals visible to the naked eye. It is found in large batholiths globally, such as the Sierra Nevada in California.