Parawulffite is a rare volcanic fumarole mineral discovered at the Tolbachik volcano in Russia. It typically appears as attractive dark green to deep emerald green 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 light green 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: dark green, deep emerald green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, subparallel aggregates.
Often confused with
Parawulffite vs. its common look-alikes, and how to tell them apart in the field.
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
- 3.35 g/cm³
- Streak
- Light Green
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Subparallel Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarole Deposits
Where rockhounds find parawulffite
Classic worldwide localities
- Tolbachik volcano, Kamchatka, Russia
Field-hunting tip
Look in fumarole deposits country, 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.

