Mertieite is a rare palladium-antimony mineral typically found as microscopic grains in ultramafic rocks or concentrated in placer deposits. It is a metallic mineral that is highly dense and usually identified through microprobe analysis due to its scarcity and lack of distinct crystal form.
Is this mertieite?
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 mertieite with a known reference. Mertieite sits at Mohs 3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Mertieite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Mertieite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, pale yellow.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: granular, irregular grains, intergrowths.
Often confused with
Mertieite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside mertieite
Minerals reported to co-occur with mertieite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pd₁₁Sb₄
- Mohs hardness
- 3.5
- Density
- 9.9-10.2 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Granular, Irregular Grains, Intergrowths
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Ultramafic Rocks, Placer Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find mertieite
Classic worldwide localities
- Goodnews Bay (Alaska, USA)
- Stillwater Complex (Montana, USA)
- Norilsk (Russia)
Field-hunting tip
Look in ultramafic rocks, placer deposits country, the host setting where mertieite typically forms. If you start seeing platinum group minerals, magnetite, chromite in float, you are in the right ground. Field specimens usually show a granular, irregular grains, intergrowths habit, so train your eye for that shape before scanning the outcrop.





