Lammerite is a rare copper arsenate mineral that occurs as small, intense green, transparent crystals in oxidized hydrothermal ore deposits. It is highly sought after by advanced collectors for its distinct color and scarcity, often found as radiating groups on a matrix of weathered sulfide ores.
Is this lammerite?
4-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 lammerite with a known reference. Lammerite sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 3Match the color rangeCompare against the expected color range: dark green.
- 4Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, radial aggregates.
Often confused with
Lammerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside lammerite
Minerals reported to co-occur with lammerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₃(AsO₄)₂
- Mohs hardness
- 3-4
- Density
- 5.18 g/cm³
- Colors
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals, radial aggregates
- Cleavage
- None observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- The product of post-eruption fumarolic reactions (400–650 °C) in an active volcano
Where rockhounds find lammerite
Classic worldwide localities
- Second Scoria cone of the Northern Branch of the Great fissure Tolbachik eruption (1975–1976), Kamchatka peninsula, Russia
Field-hunting tip
Where it forms: The product of post-eruption fumarolic reactions (400–650 °C) in an active volcano. If you start seeing euchlorine, piypite, alumokluchevskite in float, you are in the right ground. Typical habit: prismatic crystals, radial aggregates. Train your eye for that shape before scanning the outcrop.






