Diorite is a coarse-grained plutonic rock primarily composed of plagioclase feldspar and dark ferromagnesian minerals like hornblende or biotite. It lacks significant quartz, which distinguishes it visually from granite by its darker, salt-and-pepper appearance. Historically prized for its hardness, it is often found in large intrusive igneous masses.
Is this diorite?
5-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 diorite with a known reference. Diorite sits at Mohs 6-7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Diorite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Diorite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: gray, black, white.
- 5Look at form & habitTypical habit: granular.
Often confused with
Diorite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside diorite
Minerals reported to co-occur with diorite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 6-7
- Density
- 2.8-3.0 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Opaque
- Crystal habit
- Granular
- Cleavage
- None
- Rarity
- Common
- Uses
- Construction, Sculpture, Decorative
- Host rock
- Plutonic Igneous Environments
- Typical price
- $1-10 per sample
Where rockhounds find diorite
Classic worldwide localities
- Scotland
- Germany
- Finland
- Sweden
- United States
Field-hunting tip
Look in plutonic igneous environments country, the host setting where diorite typically forms. If you start seeing plagioclase, biotite, hornblende in float, you are in the right ground. Field specimens usually show a granular habit, so train your eye for that shape before scanning the outcrop.






