Kröhnkite is a rare hydrated sodium copper sulfate characterized by its distinct bright azure-blue color and vitreous luster. It forms primarily as a secondary mineral in the arid oxidation zones of copper deposits, often found as tabular crystals or fibrous crusts associated with other copper sulfates.
Is this kröhnkite?
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 kröhnkite with a known reference. Kröhnkite 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: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: blue, dark sky blue, greenish blue, yellowish green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: encrustations, fibrous, massive.
Often confused with
Kröhnkite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kröhnkite
Minerals reported to co-occur with kröhnkite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Cu(SO₄)₂·2H₂O
- Mohs hardness
- 2.5-3
- Density
- 2.90 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Encrustations, fibrous, massive
- Cleavage
- Perfect on {010}; poor on {101}
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- An uncommon secondary mineral formed in the oxidized zone of copper deposits, typically in very arid climates
Where rockhounds find kröhnkite
Classic worldwide localities
- Chuquicamata, at Quetena, west of Calama, and at Collahuasi, Antofagasta, Chile
- El Cobre de Mejillones and in the Incahuasi district, Atacama, Chile
- Wheal Hazard, St. Just, Cornwall, England
- Recsk copper deposit, Mátra Mountains, Hungary
- Capo Calamita, Elba, Italy
- Broken Hill, New South Wales, Australia
Field-hunting tip
Where it forms: An uncommon secondary mineral formed in the oxidized zone of copper deposits, typically in very arid climates. If you start seeing atacamite, blödite, chalcanthite in float, you are in the right ground. Typical habit: encrustations, fibrous, massive. Train your eye for that shape before scanning the outcrop.






