Evdokimovite is an exceptionally rare thallium-bearing sulfate mineral discovered in fumarole deposits of the Mutnovsky Volcano. It typically forms as small, vivid yellow crystalline crusts or aggregates, often associated with other rare volcanic sulfates. Due to its thallium content and exclusive occurrence in remote volcanic vents, it is highly sought after by specialized mineral collectors.
Is this evdokimovite?
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 evdokimovite with a known reference. Evdokimovite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Evdokimovite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Evdokimovite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange-yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, crusts, aggregates.
Often confused with
Evdokimovite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside evdokimovite
Minerals reported to co-occur with evdokimovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₄Tl₄(SO₄)₄
- Mohs hardness
- 2
- Density
- 2.8 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Crusts, Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarole Deposits
- Typical price
- $100-500+ depending on matrix quality
Where rockhounds find evdokimovite
Classic worldwide localities
- Mutnovsky Volcano, Kamchatka Peninsula, Russia
Field-hunting tip
Look in fumarole deposits country — that is the host setting where evdokimovite typically forms. If you start seeing thenardite, aphthitalite, krasheninnikovite in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts, aggregates habit, so train your eye for that shape before scanning the outcrop.



