Filatovite is an extremely rare arsenic-bearing feldspar found exclusively in the fumaroles of the Tolbachik volcano in Russia. It typically occurs as small, clear, tabular crystals associated with other unusual volcanic minerals. Due to its arsenic content, it is strictly a mineralogical specimen for advanced collectors and requires careful handling.
Is this filatovite?
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 filatovite with a known reference. Filatovite sits at Mohs 6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Filatovite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Filatovite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Filatovite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside filatovite
Minerals reported to co-occur with filatovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K(AlZn)₂(As,Si)₂O₈
- Mohs hardness
- 6
- Density
- 2.62 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect On {001} and {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarole Deposits of Volcanic Rocks
- Typical price
- $100-500+ for micro-specimens
Where rockhounds find filatovite
Classic worldwide localities
- Tolbachik volcano, Kamchatka Peninsula, Russia
Field-hunting tip
Look in fumarole deposits of volcanic rocks country — that is the host setting where filatovite typically forms. If you start seeing arsenatokentrolite, lammerite, sylvite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.




