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 — that is 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.






