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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine.
- 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 to translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Most likely a late-stage, low-temperature hydrothermal (epigenetic) reworking of primary Pb-Cu-Zn-Ag sulfides
Where rockhounds find vladkrivovichevite
Classic worldwide localities
- Kombat mine, Grootfontein, Namibia
Field-hunting tip
Where it forms: Most likely a late-stage, low-temperature hydrothermal (epigenetic) reworking of primary Pb-Cu-Zn-Ag sulfides. If you start seeing hereroite, asisite, damaraite in float, you are in the right ground. Typical habit: grains. Train your eye for that shape before scanning the outcrop.





