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, 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.






