Rock Identifier
Granodiorite (Phaneritic-textured Intrusive Granodiorite) — igneous
igneous

Granodiorite

Phaneritic-textured Intrusive Granodiorite

Hardness: 6-7 on Mohs scale; Color: Salt-and-pepper (mottled grey, white, and black); Luster: Dull to sub-vitreous; Crystal structure: Phaneritic (coarse-grained crystals visible to the naked eye); Specific gravity: 2.6 to 2.73.

Hardness
6-7 on Mohs scale
Color
Salt-and-pepper (mottled grey, white, and black)
Luster
Dull to sub-vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale; Color: Salt-and-pepper (mottled grey, white, and black); Luster: Dull to sub-vitreous; Crystal structure: Phaneritic (coarse-grained crystals visible to the naked eye); Specific gravity: 2.6 to 2.73.

Formation & geological history

Formed through the slow cooling of silica-rich magma deep within the Earth's crust (plutonic). It is common in continental crust and often found in mountain ranges formed by volcanic arcs. Geological age varies from Precambrian to Cenozoic depending on the specific batholith.

Uses & applications

Used widely as crushed stone for road construction and aggregate. High-quality slabs are used for countertops, building facades, and paving stones (often sold commercially as 'grey granite').

Geological facts

Granodiorite is the rock that makes up the famous Rosetta Stone and much of the Plymouth Rock. It is intermediate in composition between granite and diorite, containing more plagioclase feldspar than orthoclase feldspar.

Field identification & locations

Identify in the field by looking for a coarse grain size where white/grey plagioclase feldspar outnumbers pinkish orthoclase, mixed with dark biotite or hornblende. It is found in abundance in the Sierra Nevada mountains and other subduction zone cordilleras.