Granodiorite is a phaneritic, intrusive igneous rock similar to granite but containing more plagioclase feldspar than orthoclase. It is commonly found in large batholiths and is characterized by a salt-and-pepper appearance caused by the mixture of light-colored minerals and darker mafic components.
Is this granodiorite?
4-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch granodiorite with a known reference. Granodiorite sits at Mohs 6-7 — softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Granodiorite typically shows a vitreous luster.
- 3Match the color rangeCompare against the expected color range: gray, white, black, speckled.
- 4Look at form & habitTypical habit: phaneritic granular.
Often confused with
Granodiorite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside granodiorite
Minerals reported to co-occur with granodiorite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 6-7
- Density
- 2.65-2.75 g/cm³
- Luster
- Vitreous
- Transparency
- Opaque
- Crystal habit
- Phaneritic Granular
- Rarity
- Common
- Uses
- Construction, Architecture, Decorative
- Host rock
- Plutonic Igneous
- Typical price
- $1-10 specimen
Where rockhounds find granodiorite
Classic worldwide localities
- United States
- Canada
- Norway
- Scotland
- Australia
Field-hunting tip
Look in plutonic igneous country — that is the host setting where granodiorite typically forms. If you start seeing quartz, plagioclase, potassium feldspar in float, you are in the right ground. Field specimens usually show a phaneritic granular habit, so train your eye for that shape before scanning the outcrop.






