Parawulffite is a rare volcanic fumarole mineral discovered at the Tolbachik volcano in Russia. It typically appears as attractive blue tabular crystals associated with other copper-bearing volcanic minerals.
Is this parawulffite?
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 parawulffite with a known reference. Parawulffite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Parawulffite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Parawulffite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: blue, greenish-blue.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, subparallel aggregates.
Often confused with
Parawulffite vs. its common look-alikes — and how to tell them apart in the field.
How to tell apart: Streak differs — Parawulffite leaves white, Wulffite leaves light green.
How to tell apart: Streak differs — Parawulffite leaves white, Kamchatkite leaves yellow; luster reads vitreous on Parawulffite and resinous on Kamchatkite.
Often found alongside parawulffite
Minerals reported to co-occur with parawulffite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₅Na₃Cu₈O₂(SO₄)₄Cl₁₀
- Mohs hardness
- 3-4
- Density
- 4.26 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Subparallel Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarole Deposits
- Typical price
- $50-300 per micro-mount or small specimen
Where rockhounds find parawulffite
Classic worldwide localities
- Tolbachik volcano, Kamchatka, Russia
Field-hunting tip
Look in fumarole deposits country — that is the host setting where parawulffite typically forms. If you start seeing wulffite, kamchatkite, tolbachikite in float, you are in the right ground. Field specimens usually show a tabular crystals, subparallel aggregates habit, so train your eye for that shape before scanning the outcrop.

