Rock Identifier
Feldspar Granodiorite (Granodiorite (Na,Ca)(Si,Al)4O8) — igneous
igneous

Feldspar Granodiorite

Granodiorite (Na,Ca)(Si,Al)4O8

Hardness: 6-7 (Mohs scale); Color: Pinkish-orange with gray/white matrix; Luster: Pearly to Vitreous; Crystal Structure: Monoclinic/Triclinic; Specific Gravity: 2.6-2.7

Hardness
6-7 (Mohs scale)
Color
Pinkish-orange with gray/white matrix
Luster
Pearly to Vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 (Mohs scale); Color: Pinkish-orange with gray/white matrix; Luster: Pearly to Vitreous; Crystal Structure: Monoclinic/Triclinic; Specific Gravity: 2.6-2.7

Formation & geological history

Formed from the slow cooling of silica-rich magma beneath the Earth's surface (plutonic). Found in continental crust, often during the Paleozoic or Mesozoic eras during mountain-building events.

Uses & applications

Crushed stone for road construction, building materials, ornamental stone, and occasionally used as a soil conditioner when ground.

Geological facts

Granodiorite is the most common intrusive rock in the Earth's crust; the famous Rosetta Stone was actually carved on a slab of granodiorite.

Field identification & locations

Identify by its interlocking crystalline texture and coarse grain size. Look for the distinct cleavage of feldspar crystals (two planes at near 90 degrees). Commonly found in batholiths and large mountain ranges like the Sierra Nevada.