Fedotovite is a rare copper sulfate mineral formed by volcanic fumarolic activity. It is characterized by its distinct green to bluish-green tabular crystals and is found primarily in the vents of the Tolbachik volcano.
Is this fedotovite?
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 fedotovite with a known reference. Fedotovite 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. Fedotovite leaves a greenish-white streak.
- 3Read the lusterHold the specimen under a strong light. Fedotovite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, bluish-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, incrustations.
Often confused with
Fedotovite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Fedotovite leaves greenish-white, Euchlorine leaves pale green.
How to tell apart: Streak differs, so Fedotovite leaves greenish-white, Kamchatkite leaves yellow; luster reads vitreous on Fedotovite and resinous on Kamchatkite.
Often found alongside fedotovite
Minerals reported to co-occur with fedotovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂Cu₃O(SO₄)₃
- Mohs hardness
- 2-3
- Density
- 3.32 g/cm³
- Colors
- Streak
- Greenish-white
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Incrustations
- Cleavage
- Perfect On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarolic Deposits
- Typical price
- $50-500 depending on specimen size and quality
Where rockhounds find fedotovite
Classic worldwide localities
- Tolbachik volcano, Kamchatka Peninsula, Russia
Field-hunting tip
Look in fumarolic deposits country, the host setting where fedotovite typically forms. If you start seeing tenorite, langbeinite, sylvite in float, you are in the right ground. Field specimens usually show a tabular crystals, incrustations habit, so train your eye for that shape before scanning the outcrop.




