Potarite is a rare palladium-mercury intermetallic compound found primarily in alluvial diamond-bearing gravels. It typically occurs as small, silvery-white metallic grains or nuggets that are notable for their unusually high density due to their mercury content.
Is this potarite?
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 potarite with a known reference. Potarite sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Potarite leaves a silver-white streak.
- 3Read the lusterHold the specimen under a strong light. Potarite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, silver-white.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: grains, small nuggets, massive.
Often confused with
Potarite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside potarite
Minerals reported to co-occur with potarite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PdHg
- Mohs hardness
- 3.5-4
- Density
- 15.0-16.0 g/cm³
- Colors
- Streak
- Silver-white
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Grains, Small Nuggets, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Study
- Host rock
- Alluvial Deposits, Ultramafic Igneous Rocks
- Typical price
- $100-500+ depending on size and provenance
Where rockhounds find potarite
Classic worldwide localities
- Potaro River, Guyana
- Itabira, Brazil
- Koryak Mountains, Russia
- Bushveld Complex, South Africa
Field-hunting tip
Look in alluvial deposits, ultramafic igneous rocks country — that is the host setting where potarite typically forms. If you start seeing gold, platinum, hematite in float, you are in the right ground. Field specimens usually show a grains, small nuggets, massive habit, so train your eye for that shape before scanning the outcrop.






