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, 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.






