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

Granodiorite

Phaneritic Plutonic Intermediate-Felsic Rock

Hardness: 6-7 Mohs; Color: Salt and pepper (mottled gray, white, and pinkish/red); Luster: Dull to vitreous; Structure: Phaneritic (coarse-grained); Specific Gravity: 2.6-2.7

Hardness
6-7 Mohs
Color
Salt and pepper (mottled gray, white, and pinkish/red)
Luster
Dull to vitreous
Identified More igneous
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Physical properties

Hardness: 6-7 Mohs; Color: Salt and pepper (mottled gray, white, and pinkish/red); Luster: Dull to vitreous; Structure: Phaneritic (coarse-grained); Specific Gravity: 2.6-2.7

Formation & geological history

Formed through slow crystallization of silica-rich magma beneath the Earth's surface during the cooling of continental crust, typically in subduction zones.

Uses & applications

Used primarily in construction as crushed stone or road base, and polished for use as architectural stone, countertops, or paving.

Geological facts

Granodiorite was used by the ancient Egyptians for statues and sarcophagi. The most famous artifact made of granodiorite is the Rosetta Stone.

Field identification & locations

Identify by its interlocking crystalline texture containing both light (plagioclase, quartz) and dark (biotite, hornblende) minerals. Widely found in massive batholiths like the Sierra Nevada.