Guanacoite is a very rare copper-magnesium arsenate mineral found primarily in the oxidation zones of arsenic-rich ore deposits. It typically forms delicate pale pink tabular crystals or radial clusters and is highly prized by advanced mineral collectors for its scarcity and aesthetic crystal form.
Is this guanacoite?
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 guanacoite with a known reference. Guanacoite 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. Guanacoite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Guanacoite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pale pink, pinkish-white, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, radial aggregates, crusts.
Often confused with
Guanacoite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Streak differs — Guanacoite leaves white, Clinoclase leaves bluish-green.

How to tell apart: Conichalcite is the harder of the two (Mohs 4.5 vs. 3.5); streak differs — Guanacoite leaves white, Conichalcite leaves light green.
Often found alongside guanacoite
Minerals reported to co-occur with guanacoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₂Cu₆(AsO₄)₄(OH)₄·5H₂O
- Mohs hardness
- 3.5
- Density
- 3.2 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Radial Aggregates, Crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $50-300 per specimen
Where rockhounds find guanacoite
Classic worldwide localities
- Guanaco Mine, Antofagasta, Chile
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where guanacoite typically forms. If you start seeing austinite, quartz, arsenates in float, you are in the right ground. Field specimens usually show a tabular crystals, radial aggregates, crusts habit, so train your eye for that shape before scanning the outcrop.


