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, 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.


