Vladkrivovichevite is a rare lead manganese borate that forms grains. It was approved as a distinct mineral species in 2011. It was first described from Kombat mine, Grootfontein, Namibia.
Is this vladkrivovichevite?
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 vladkrivovichevite with a known reference. Vladkrivovichevite 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. Vladkrivovichevite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Vladkrivovichevite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: pale greenish yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: grains.
Often confused with
Vladkrivovichevite vs. its common look-alikes, and how to tell them apart in the field.
How to tell apart: Krivovichevite is the harder of the two (Mohs 3 vs. 2); luster reads adamantine on Vladkrivovichevite and vitreous on Krivovichevite.

How to tell apart: Laurionite is the harder of the two (Mohs 3-3.5 vs. 2).
Often found alongside vladkrivovichevite
Minerals reported to co-occur with vladkrivovichevite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- [Pb₃₂O₁₈][Pb₄Mn₂O]Cl₁₄(BO₃)₈·2H₂O
- Mohs hardness
- 2
- Density
- 7.40 g/cm³
- Colors
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarole Deposits
Where rockhounds find vladkrivovichevite
Classic worldwide localities
- Kombat mine, Grootfontein, Namibia
Field-hunting tip
Look in fumarole deposits country, the host setting where vladkrivovichevite typically forms. If you start seeing sylvite, halite, anglesite in float, you are in the right ground. Field specimens usually show a grains habit, so train your eye for that shape before scanning the outcrop.




