Kolovratite is a rare, amorphous zinc-nickel-copper vanadate that typically forms as earthy crusts or thin coatings on host rock. It is primarily identified by its characteristic yellowish to greenish-yellow color within oxidized vanadium-rich deposits. Due to its rarity and obscure nature, it is sought after primarily by advanced collectors of secondary vanadium minerals.
Is this kolovratite?
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 kolovratite with a known reference. Kolovratite sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kolovratite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Kolovratite typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-green.
- 5Look at form & habitCrystal system: amorphous. Typical habit: crusts, reniform, earthy masses.
Often confused with
Kolovratite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside kolovratite
Minerals reported to co-occur with kolovratite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Zn,Ni,Cu)₃(VO₄)₂·nH₂O
- Mohs hardness
- 2-3
- Density
- 2.8 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Dull
- Transparency
- Opaque
- Crystal system
- Amorphous
- Crystal habit
- Crusts, Reniform, Earthy Masses
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sedimentary Oxidized Zone of Uranium-vanadium Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find kolovratite
Classic worldwide localities
- Ferghana Valley, Uzbekistan
- Tyuya-Muyun, Kyrgyzstan
Field-hunting tip
Look in sedimentary oxidized zone of uranium-vanadium deposits country — that is the host setting where kolovratite typically forms. If you start seeing tyuyamunite, vanadinite, calcite in float, you are in the right ground. Field specimens usually show a crusts, reniform, earthy masses habit, so train your eye for that shape before scanning the outcrop.




