Coldwellite is a rare palladium-antimony mineral primarily identified from the Coldwell Complex in Ontario. It typically occurs as microscopic anhedral grains associated with other base-metal sulfides and platinum-group minerals in alkaline igneous rocks.
Is this coldwellite?
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 coldwellite with a known reference. Coldwellite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Coldwellite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Coldwellite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, pale yellow.
- 5Look at form & habitCrystal system: cubic. Typical habit: anhedral grains.
Often confused with
Coldwellite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside coldwellite
Minerals reported to co-occur with coldwellite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pd₃Sb
- Mohs hardness
- 3-4
- Density
- 9.52 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Complex
- Typical price
- n/a
Where rockhounds find coldwellite
Classic worldwide localities
- Coldwell Complex, Ontario, Canada
Field-hunting tip
Look in alkaline igneous complex country — that is the host setting where coldwellite typically forms. If you start seeing chalcopyrite, magnetite, ilmenite 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.




