Eskimoite is a rare sulfosalt mineral primarily known from its type locality in the cryolite deposits of Ivigtut, Greenland. It typically occurs as small, needle-like acicular crystals or massive metallic aggregates within hydrothermal environments associated with lead and bismuth sulfides.
Is this eskimoite?
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 eskimoite with a known reference. Eskimoite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Eskimoite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Eskimoite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: lead-gray, steel-gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular crystals, granular aggregates, massive.
Often confused with
Eskimoite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside eskimoite
Minerals reported to co-occur with eskimoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₂Pb₃Bi₄S₉
- Mohs hardness
- 2.5-3
- Density
- 6.8-7.0 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular Crystals, Granular Aggregates, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins, Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find eskimoite
Classic worldwide localities
- Ivigtut (Ivittuut), Greenland
- Bolivia
- Czech Republic
Field-hunting tip
Look in hydrothermal veins, pegmatites country — that is the host setting where eskimoite typically forms. If you start seeing galena, siderite, fluorite in float, you are in the right ground. Field specimens usually show a acicular crystals, granular aggregates, massive habit, so train your eye for that shape before scanning the outcrop.






