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. Karpovite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Karpovite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: white.
- 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
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Sheaf-like Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites
Where rockhounds find karpovite
Classic worldwide localities
- Khibiny Massif, Russia
- Lovozero Massif, Russia
Field-hunting tip
Look in alkaline pegmatites country, the host setting where karpovite typically forms. If you start seeing anatase, apatite, microcline in float, you are in the right ground. Field specimens usually show a sheaf-like aggregates habit, so train your eye for that shape before scanning the outcrop.





