Granodiorite
Granodiorite (Intermediate intrusive igneous rock)
Rock Type: igneous

Physical Properties
Hardness: 6-7 (Mohs scale); Color: Salt-and-pepper (white, grey, black); Luster: Phaneritic (crystalline); Crystal structure: Granular/Coarse-grained; Specific gravity: approx. 2.6-2.7
Formation & Geological History
Formed from the slow cooling of silica-rich magma beneath the Earth's surface. Often associated with continental arc magmatism and mountain building (orogeny) during various geological eras from the Precambrian to Cenozoic.
Uses & Applications
Commonly used in construction as crushed stone or 'granite' countertops, paving stones, and memorial monuments. It is also a source rock for various metallic ores.
Geological Facts
Granodiorite is the most common intrusive rock found in the Earth's continental crust. Famous examples include the Rosetta Stone, which was carved into a block of granodiorite, and many of the peaks in the Sierra Nevada batholith.
Field Identification & Locations
Identify in the field by its medium-to-coarse-grained 'salt-and-pepper' appearance. Unlike true granite, it contains more plagioclase feldspar than orthoclase. Found in large batholiths globally.
Identified on: 4/17/2026
Mode: Standard