Falgarite is a rare potassium vanadium sulfate that forms turquoise isometric or pseudo-octahedral individual crystals. It is a fumarolic, formed directly from gas emitted by a natural underground coal fire. It was first described from Kuhi-Malik gorge near Ravat kishlak, Fan-Yagnob coal deposit, ~100 km north of Dushanbe, Tajikistan.
Is this falgarite?
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 falgarite with a known reference. Falgarite 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. Falgarite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Falgarite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: turquoise, green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: isometric or pseudo-octahedral individual crystals.
Often confused with
Falgarite vs. its common look-alikes, and how to tell them apart in the field.
All properties
- Chemical formula
- K₄(VO)₃(SO₄)₅
- Mohs hardness
- 2-3
- Density
- 2.87 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Isometric or Pseudo-octahedral Individual Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Sedimentary Deposits
Where rockhounds find falgarite
Classic worldwide localities
- Kuhi-Malik gorge near Ravat kishlak, Fan-Yagnob coal deposit, Tajikistan
Field-hunting tip
Look in sedimentary deposits country, the host setting where falgarite typically forms. If you start seeing sand, soil components in float, you are in the right ground. Field specimens usually show a isometric or pseudo-octahedral individual crystals habit, so train your eye for that shape before scanning the outcrop.


