Vlodavetsite is a rare lead-calcium arsenate-sulfate chloride found primarily in volcanic fumaroles. It typically occurs as tiny, thin tabular crystals formed through sublimation and direct deposition from volcanic gases.
Is this vlodavetsite?
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 vlodavetsite with a known reference. Vlodavetsite 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: colorless, yellow white.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: platy, tabular.
Often confused with
Vlodavetsite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside vlodavetsite
Minerals reported to co-occur with vlodavetsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Al(SO₄)₂F₂Cl·4H₂O
- Mohs hardness
- 2-3
- Density
- 2.35 g/cm³
- Colors
- ColorlessYellow white
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Tetragonal
- Crystal habit
- Platy, tabular
- Cleavage
- On {100}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A product of low-temperature hydration of minerals on the fracture walls of volcanic fumaroles
Where rockhounds find vlodavetsite
Classic worldwide localities
- Tolbachik fissure volcano, Kamchatka Peninsula, Russia
Field-hunting tip
Where it forms: A product of low-temperature hydration of minerals on the fracture walls of volcanic fumaroles. If you start seeing gypsum, sellaite, bischofite in float, you are in the right ground. Typical habit: platy, tabular. Train your eye for that shape before scanning the outcrop.






