Rock Identifier
Granodiorite (Granodiorite (containing Plagioclase, Quartz, Orthoclase, Biotic/Hornblende)) — igneous
igneous

Granodiorite

Granodiorite (containing Plagioclase, Quartz, Orthoclase, Biotic/Hornblende)

Hardness: 6-7 Mohs; Color: Salt and pepper (white/grey with black speckles); Luster: Phaneritic (crystalline); Structure: Massive, granular; Specific Gravity: 2.6-2.7

Hardness
6-7 Mohs
Color
Salt and pepper (white/grey with black speckles)
Luster
Phaneritic (crystalline)
Identified More igneous
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Physical properties

Hardness: 6-7 Mohs; Color: Salt and pepper (white/grey with black speckles); Luster: Phaneritic (crystalline); Structure: Massive, granular; Specific Gravity: 2.6-2.7

Formation & geological history

Formed by the slow cooling of silica-rich magma beneath the Earth's surface in continental crust environments, typically in volcanic arcs and mountain building zones.

Uses & applications

Used widely in construction as crushed stone, road grade, and as ornamental building stone (sold commercially as 'white granite' for countertops and flooring).

Geological facts

Granodiorite is the intermediate rock between granite and diorite. The famous Rosetta Stone was carved from a slab of granodiorite, not basalt as originally thought.

Field identification & locations

Identify by looking for a coarse-grained texture where the white/grey plagioclase feldspar crystals outnumber the pinkish orthoclase. Found in large batholiths like the Sierra Nevada.