Krivovichevite is a rare lead-aluminum tellurite sulfate mineral discovered in the fumaroles of the Tolbachik volcano. It typically occurs as small, delicate, transparent to translucent platy crystals within volcanic vent deposits.
Is this krivovichevite?
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 krivovichevite with a known reference. Krivovichevite 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. Krivovichevite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Krivovichevite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals.
Often confused with
Krivovichevite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside krivovichevite
Minerals reported to co-occur with krivovichevite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₃Al₂[(OH)₄|TeO₃]₂(SO₄)·3H₂O
- Mohs hardness
- 2
- Density
- 5.02 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarolic Deposits
Where rockhounds find krivovichevite
Classic worldwide localities
- Tolbachik volcano, Kamchatka Peninsula, Russia
Field-hunting tip
Look in fumarolic deposits country, the host setting where krivovichevite typically forms. If you start seeing anglesite, sillenite, gold in float, you are in the right ground. Field specimens usually show a platy crystals habit, so train your eye for that shape before scanning the outcrop.




