Tredouxite is a rare nickel antimony oxide, typically black. It occurs in a podiform nickeliferous deposit in altered ultramafic rocks. It is associated with trevorite and bottinoite. It was first described from Bon Accord Ni-oxide deposit, southeast of Nelspruit, Republic of South Africa.
Is this tredouxite?
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 tredouxite with a known reference. Tredouxite sits at Mohs 3-3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Tredouxite leaves a gray streak.
- 3Read the lusterHold the specimen under a strong light. Tredouxite typically shows a submetallic luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: anhedral grains.
Often confused with
Tredouxite vs. its common look-alikes, and how to tell them apart in the field.
How to tell apart: Manaccanite is the harder of the two (Mohs 5-6 vs. 3-3.5); streak differs, so Tredouxite leaves gray, Manaccanite leaves black.

How to tell apart: Magnetite is the harder of the two (Mohs 5.5-6.5 vs. 3-3.5); streak differs, so Tredouxite leaves gray, Magnetite leaves black; luster reads submetallic on Tredouxite and metallic to submetallic to dull on Magnetite.
Often found alongside tredouxite
Minerals reported to co-occur with tredouxite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NiSb₂O₆
- Mohs hardness
- 3-3.5
- Density
- 6.650 g/cm³
- Colors
- Streak
- Gray
- Luster
- Submetallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Ultramafic Rocks
Where rockhounds find tredouxite
Classic worldwide localities
- Bon Accord nickel deposit, South Africa
Field-hunting tip
Look in ultramafic rocks country, the host setting where tredouxite typically forms. If you start seeing trevorite, willemseite, bunsenite in float, you are in the right ground. Field specimens usually show a anhedral grains habit, so train your eye for that shape before scanning the outcrop.



