Badalovite is a rare member of the garnet group characterized by high vanadium content within its structure. It typically occurs as small dodecahedral crystals in metasomatic environments and is primarily sought after by advanced systematic mineral collectors due to its restricted occurrence.
Is this badalovite?
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 badalovite with a known reference. Badalovite sits at Mohs 7-7.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Badalovite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Badalovite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: dark brown, reddish-brown.
- 5Look at form & habitCrystal system: cubic. Typical habit: dodecahedral crystals.
Often confused with
Badalovite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside badalovite
Minerals reported to co-occur with badalovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃(V³⁺,Mg,Fe³⁺)₂(SiO₄)₃
- Mohs hardness
- 7-7.5
- Density
- 3.8-3.9 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Dodecahedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Mineralogical Research
- Host rock
- Metasomatic Rocks
- Typical price
- $100-500+ per specimen
Where rockhounds find badalovite
Classic worldwide localities
- Kurumsak, Uzbekistan
Field-hunting tip
Look in metasomatic rocks country — that is the host setting where badalovite typically forms. If you start seeing calcite, quartz, vanadiferous minerals in float, you are in the right ground. Field specimens usually show a dodecahedral crystals habit, so train your eye for that shape before scanning the outcrop.




