Magnesiocopiapite is a secondary sulfate mineral that typically forms as an efflorescent crust or thin coating in the weathering zones of sulfide deposits. It is best identified by its bright yellow color and occurrence alongside other iron-sulfates; it is highly water-soluble and should be kept dry.
Is this magnesiocopiapite?
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 magnesiocopiapite with a known reference. Magnesiocopiapite sits at Mohs 2.5-3, 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, green yellow, yellow green, orange.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals, granular crusts, efflorescent aggregates.
Often confused with
Magnesiocopiapite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside magnesiocopiapite
Minerals reported to co-occur with magnesiocopiapite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MgFe₄³⁺(SO₄)₆(OH)₂·20H₂O
- Mohs hardness
- 2.5-3
- Density
- 2.08-2.17 g/cm³
- Streak
- Light yellow
- Luster
- Pearly
- Transparency
- Semitransparent
- Crystal system
- Triclinic
- Crystal habit
- Platy crystals, granular crusts, efflorescent aggregates
- Cleavage
- On {010}, perfect (by analogy to copiapite group members)
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- An uncommon secondary mineral, typically formed by oxidation of pyrite
Where rockhounds find magnesiocopiapite
Classic worldwide localities
- Blythe, Riverside Co., and at the Redington mercury mine, Knoxville, Napa Co., California, USA
- Las Vegas, Tecolote district, San Miguel Co., New Mexico, USA
- Denver mine, Santa Cruz Co., and the United Verde mine, Jerome, Yavapai Co., Arizona, USA
- A prospect pit along the Mosquito Fork, Forty Mile River, Eagle A-3 quadrangle, Alaska, USA
- Prince mine, Cape Breton Island, Nova Scotia, Canada
- Falun, Kopparberg, Sweden
Field-hunting tip
Where it forms: An uncommon secondary mineral, typically formed by oxidation of pyrite. If you start seeing pyrite, römerite, paracoquimbite in float, you are in the right ground. Typical habit: platy crystals, granular crusts, efflorescent aggregates. Train your eye for that shape before scanning the outcrop.







