Karpovite is a rare thallium vanadium sulfate that forms sheaf-like aggregates. It is a sublimate on rock around a volcanic fumarole. Associated minerals include shcherbinaite, pauflerite and bobjonesite. It was first described from First cinder cone, North Breach of the Great Fissure Tolbachik volcano, Kamchatka Peninsula, Russia.
Is this karpovite?
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 karpovite with a known reference. Karpovite 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: white.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine.
- 4Match the color rangeCompare against the expected color range: white with a bluish tint.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: sheaf-like aggregates.
Often confused with
Karpovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside karpovite
Minerals reported to co-occur with karpovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Tl₂VO(SO₄)₂(H₂O)
- Mohs hardness
- ~2
- Density
- 4.743 g/cm³
- Colors
- White with a bluish tint
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Sheaf-like aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A sublimate on rock around a volcanic fumarole
Where rockhounds find karpovite
Classic worldwide localities
- First cinder cone, North Breach of the Great Fissure Tolbachik volcano, Kamchatka Peninsula, Russia
Field-hunting tip
Where it forms: A sublimate on rock around a volcanic fumarole. If you start seeing shcherbinaite, pauflerite, bobjonesite in float, you are in the right ground. Typical habit: sheaf-like aggregates. Train your eye for that shape before scanning the outcrop.


