Ericlaxmanite is an extremely rare copper magnesium arsenate mineral discovered in the volcanic fumaroles of the Tolbachik volcano. It typically forms as thin tabular crystals or delicate crusts associated with other complex copper-rich volcanic minerals.
Is this ericlaxmanite?
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 ericlaxmanite with a known reference. Ericlaxmanite sits at Mohs ~3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: light green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: dark green, green.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, crystalline crusts.
Often confused with
Ericlaxmanite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ericlaxmanite
Minerals reported to co-occur with ericlaxmanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₄O(AsO₄)₂
- Mohs hardness
- ~3.5
- Density
- 5.036 g/cm³
- Colors
- Streak
- Light green
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals, crystalline crusts
- Cleavage
- Distinct, one direction (observed under the microscope)
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As complex incrustations on the surface of basalt scoria or in open pockets
Where rockhounds find ericlaxmanite
Classic worldwide localities
- Arsenatnaya fumarole, Second scoria cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia
Field-hunting tip
Where it forms: As complex incrustations on the surface of basalt scoria or in open pockets. If you start seeing kozyrevskite, urusovite, lammerite in float, you are in the right ground. Typical habit: tabular crystals, crystalline crusts. Train your eye for that shape before scanning the outcrop.



