Kudriavite is an extremely rare cadmium-lead bismuth sulfide mineral found in volcanic fumaroles. It typically forms as small, yellowish, metallic platy crystals occurring within the mineralized vents of high-temperature volcanoes.
Is this kudriavite?
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 kudriavite with a known reference. Kudriavite sits at Mohs 2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: dark reddish gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy.
Often confused with
Kudriavite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kudriavite
Minerals reported to co-occur with kudriavite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Cd,Pb)Bi₂S₄
- Mohs hardness
- 2
- Density
- 6.578 g/cm³
- Colors
- Dark reddish gray
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Platy
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As high-temperature (~ 400 °C) fumarole encrustations on the inner wall of an active andesitic stratovolcanic crater
Where rockhounds find kudriavite
Classic worldwide localities
- Kudriavy volcano, Iturup Island, Kurile arc, Russia
Field-hunting tip
Where it forms: As high-temperature (~ 400 °C) fumarole encrustations on the inner wall of an active andesitic stratovolcanic crater. If you start seeing cannizzarite, greenockite, pyrite in float, you are in the right ground. Typical habit: platy. Train your eye for that shape before scanning the outcrop.






