Chrysothallite is a rare secondary mineral found in high-temperature fumaroles of volcanic systems. It typically occurs as delicate, bright green to yellow-green platy crystals or thin crusts associated with other exotic copper-bearing chlorides and selenites.
Is this chrysothallite?
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 chrysothallite with a known reference. Chrysothallite 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. Chrysothallite leaves a pale green streak.
- 3Read the lusterHold the specimen under a strong light. Chrysothallite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, yellow-green.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: platy crystals, crusts.
Often confused with
Chrysothallite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside chrysothallite
Minerals reported to co-occur with chrysothallite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₆Cu₆O₂Cl₁₀(SeO₃)₄
- Mohs hardness
- 2
- Density
- 4.26 g/cm³
- Colors
- Streak
- Pale Green
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Platy Crystals, Crusts
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarole Deposits
- Typical price
- n/a
Where rockhounds find chrysothallite
Classic worldwide localities
- Tolbachik volcano, Kamchatka Peninsula, Russia
Field-hunting tip
Look in fumarole deposits country — that is the host setting where chrysothallite typically forms. If you start seeing sylvite, halite, euchlorine in float, you are in the right ground. Field specimens usually show a platy crystals, crusts habit, so train your eye for that shape before scanning the outcrop.




