Dantopaite is a rare silver bismuth selenide discovered in the Dantopa deposit of Argentina. It typically occurs as small grains associated with other selenide minerals in hydrothermal environments, requiring microscopic identification techniques to confirm.
Is this dantopaite?
4-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 dantopaite with a known reference. Dantopaite sits at Mohs 3.5, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: metallic.
- 3Match the color rangeCompare against the expected color range: dark gray, black.
- 4Look at form & habitCrystal system: monoclinic. Typical habit: anhedral grains, irregular masses.
Often confused with
Dantopaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside dantopaite
Minerals reported to co-occur with dantopaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₅Bi₁₃S₂₂
- Mohs hardness
- 3.5
- Density
- 6.74 g/cm³
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Anhedral grains, irregular masses
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- From mineralized (metallic sulfosalts) hydrothermal quartz veins
Where rockhounds find dantopaite
Classic worldwide localities
- Erzwies mining district, Hohe Tauern region, west of the Gasteinertal, province of Salzburg, Austria
Field-hunting tip
Where it forms: From mineralized (metallic sulfosalts) hydrothermal quartz veins. If you start seeing bismuthinite, krupkaite, pavonite in float, you are in the right ground. Typical habit: anhedral grains, irregular masses. Train your eye for that shape before scanning the outcrop.







