Cuprocopiapite is a rare copper-bearing member of the copiapite group formed by the oxidation of iron and copper sulfide minerals. It typically presents as yellow to greenish-yellow crusts or small, platy crystal aggregates in arid mining environments. Collectors should be aware that like other hydrous sulfates, it is water-soluble and should be stored in a dry environment.
Is this cuprocopiapite?
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 cuprocopiapite with a known reference. Cuprocopiapite sits at Mohs 2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: light yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: pearly.
- 4Match the color rangeCompare against the expected color range: yellow, greenish yellow, orange.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals, granular crusts, powdery efflorescences.
Often confused with
Cuprocopiapite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Cuprocopiapite leaves light yellow, Copiapite leaves pale yellow.

How to tell apart: Streak differs, so Cuprocopiapite leaves light yellow, Fibroferrite leaves white.

How to tell apart: Cuprocopiapite is noticeably harder (Mohs 2.5 vs. 1.5); streak differs, so Cuprocopiapite leaves light yellow, Halotrichite leaves white; luster reads pearly on Cuprocopiapite and vitreous on Halotrichite.
Often found alongside cuprocopiapite
Minerals reported to co-occur with cuprocopiapite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuFe₄(SO₄)₆(OH)₂·20H₂O
- Mohs hardness
- 2.5
- Density
- 2.23 g/cm³
- Streak
- Light yellow
- Luster
- Pearly
- Transparency
- Semitransparent
- Crystal system
- Triclinic
- Crystal habit
- Platy crystals, granular crusts, powdery efflorescences
- Cleavage
- 010, perfect; 101 imperfect (by analogy with copiapite)
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral probably formed by reaction between copiapite and copper sulfate-bearing solutions, preserved in arid climates
Where rockhounds find cuprocopiapite
Classic worldwide localities
- Chuquicamata and at Quetena, west of Calama, Antofagasta, Chile
Field-hunting tip
Where it forms: A rare secondary mineral probably formed by reaction between copiapite and copper sulfate-bearing solutions, preserved in arid climates. If you start seeing copiapite, parabutlerite, chalcanthite in float, you are in the right ground. Typical habit: platy crystals, granular crusts, powdery efflorescences. Train your eye for that shape before scanning the outcrop.



