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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 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
Where it forms: sedimentary deposits. If you start seeing sand, soil components in float, you are in the right ground. Typical habit: isometric or pseudo-octahedral individual crystals. Train your eye for that shape before scanning the outcrop.


