Colinowensite is a rare copper sulfate chloride mineral discovered in the volcanic fumaroles of the Tolbachik volcano in Russia. It typically appears as small, transparent yellow tabular crystals associated with other copper-bearing volcanic minerals.
Is this colinowensite?
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 colinowensite with a known reference. Colinowensite sits at Mohs 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Colinowensite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Colinowensite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brownish-yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals.
Often confused with
Colinowensite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside colinowensite
Minerals reported to co-occur with colinowensite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KCu₃(SO₄)₂Cl
- Mohs hardness
- 3
- Density
- 2.8 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarole Deposits of Volcanic Vents
- Typical price
- $100-500 per specimen
Where rockhounds find colinowensite
Classic worldwide localities
- Tolbachik volcano, Kamchatka, Russia
Field-hunting tip
Look in fumarole deposits of volcanic vents country — that is the host setting where colinowensite typically forms. If you start seeing fedotovite, kamchatkite, tenorite 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.


