Badalovite is a rare sodium magnesium iron arsenate that forms obliquely terminated prismatic crystals. It is a sublimate at an active volcanic fumarole. It was first described from the Arsenatnaya fumarole, Tolbachik Volcano, Kamchatka, Russia.
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: pale green, green, greenish gray, gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: obliquely terminated prismatic 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
- NaNaMg(MgFe³⁺)(AsO₄)₃
- Mohs hardness
- 7-7.5
- Density
- 4.016 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Obliquely Terminated Prismatic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Mineralogical Research
- Host rock
- Metasomatic Rocks
Where rockhounds find badalovite
Classic worldwide localities
- Arsenatnaya fumarole, Kamchatka, Russia
Field-hunting tip
Look in metasomatic rocks country, 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 obliquely terminated prismatic crystals habit, so train your eye for that shape before scanning the outcrop.




