Lapeyreite is a very rare copper arsenate mineral known primarily from its type locality in Utah. It typically occurs as small, delicate, dark pistachio-green bladed crystals often associated with other rare copper secondary minerals in oxidized hydrothermal zones.
Is this lapeyreite?
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 lapeyreite with a known reference. Lapeyreite 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. Streak: yellowish green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to adamantine.
- 4Match the color rangeCompare against the expected color range: dark pistachio-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: bladed crystals, aggregates.
Often confused with
Lapeyreite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside lapeyreite
Minerals reported to co-occur with lapeyreite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₃O[AsO₃(OH)]₂·H₂O
- Mohs hardness
- 3
- Density
- 4.385 g/cm³
- Colors
- Dark pistachio-green
- Streak
- Yellowish green
- Luster
- Vitreous to adamantine
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Bladed crystals, aggregates
- Cleavage
- Perfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral in geodes of cuprite in a weathering zone
Where rockhounds find lapeyreite
Classic worldwide localities
- Roua, Dôme de Barrot, Departement Alpes-Maritimes, France (type locality)
Field-hunting tip
Where it forms: A secondary mineral in geodes of cuprite in a weathering zone. If you start seeing trippkeite, olivenite, malachite in float, you are in the right ground. Typical habit: bladed crystals, aggregates. Train your eye for that shape before scanning the outcrop.






