Johillerite is an exceptionally rare arsenate mineral known primarily from the fumaroles of the Tolbachik volcano in Russia. It typically appears as small, tabular, yellow to yellow-green crystals formed during high-temperature volcanic activity.
Is this johillerite?
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 johillerite with a known reference. Johillerite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Johillerite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Johillerite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Johillerite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Tilasite is the harder of the two (Mohs 5 vs. 3.5); streak differs — Johillerite leaves yellow, Tilasite leaves white.

How to tell apart: Berzeliite is the harder of the two (Mohs 5 vs. 3.5); streak differs — Johillerite leaves yellow, Berzeliite leaves white.
Often found alongside johillerite
Minerals reported to co-occur with johillerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCuMg₃(AsO₄)₃
- Mohs hardness
- 3.5
- Density
- 3.44 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarolic Deposits
- Typical price
- $100-500 thumbnail
Where rockhounds find johillerite
Classic worldwide localities
- Tolbachik volcano, Russia
Field-hunting tip
Look in fumarolic deposits country — that is the host setting where johillerite typically forms. If you start seeing tenorite, hematite, paratacamite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.



