Piypite is a rare potassium copper sulfate mineral first described from the fumaroles of the Tolbachik volcano in Russia. It typically appears as bright yellow to yellow-green encrustations or delicate crystalline aggregates formed by volcanic gases.
Is this piypite?
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 piypite with a known reference. Piypite 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. Piypite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Piypite typically shows a resinous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-green.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: crusts, aggregates, small tabular crystals.
Often confused with
Piypite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Piypite leaves yellow, Euchlorine leaves pale green; luster reads resinous on Piypite and vitreous on Euchlorine.

How to tell apart: Streak differs, so Piypite leaves yellow, Chlorothionite leaves white; luster reads resinous on Piypite and vitreous on Chlorothionite.
Often found alongside piypite
Minerals reported to co-occur with piypite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₄Cu₄O₂(SO₄)₄
- Mohs hardness
- 2-3
- Density
- 3.3-3.4 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Resinous
- Transparency
- Translucent
- Crystal system
- Tetragonal
- Crystal habit
- Crusts, Aggregates, Small Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarole Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find piypite
Classic worldwide localities
- Tolbachik volcano, Kamchatka Peninsula, Russia
Field-hunting tip
Look in fumarole deposits country, the host setting where piypite typically forms. If you start seeing tenorite, sylvite, halenite in float, you are in the right ground. Field specimens usually show a crusts, aggregates, small tabular crystals habit, so train your eye for that shape before scanning the outcrop.


