Aleutite is an extremely rare copper arsenate mineral found as a result of volcanic fumarole activity. It typically occurs as tiny, dark, tabular crystals or crusts within specific high-temperature environments in the Kamchatka region.
Is this aleutite?
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 aleutite with a known reference. Aleutite sits at Mohs 2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: reddish black.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine.
- 4Match the color rangeCompare against the expected color range: dark green, black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, crusts.
Often confused with
Aleutite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside aleutite
Minerals reported to co-occur with aleutite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- [Cu₅O₂](AsO₄)(VO₄)·(Cu₀.₅☐₀.₅)Cl
- Mohs hardness
- 2
- Density
- 4.89 g/cm³
- Colors
- Streak
- Reddish black
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals, crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- fumarole deposits
Where rockhounds find aleutite
Classic worldwide localities
- Tolbachik volcano, Kamchatka, Russia
Field-hunting tip
Where it forms: fumarole deposits. If you start seeing lammerite, tenorite, sylvite in float, you are in the right ground. Typical habit: tabular crystals, crusts. Train your eye for that shape before scanning the outcrop.




