Lapeyreite is a very rare copper arsenate mineral known primarily from its type locality in Utah. It typically occurs as small, delicate, pale blue 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. Lapeyreite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Lapeyreite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: blue, pale blue.
- 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(AsO₄)(OH)₃
- Mohs hardness
- 3
- Density
- 3.32 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Bladed Crystals, Aggregates
- Cleavage
- Good in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Mineralized Veins
- Typical price
- $50-300 per specimen
Where rockhounds find lapeyreite
Classic worldwide localities
- La Sal Mountains, Utah, USA
Field-hunting tip
Look in hydrothermal mineralized veins country — that is the host setting where lapeyreite typically forms. If you start seeing tyrolite, clinoclase, azurite in float, you are in the right ground. Field specimens usually show a bladed crystals, aggregates habit, so train your eye for that shape before scanning the outcrop.



