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. Kröhnkite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Kröhnkite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: blue, blue-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, fibrous, crusts, 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
- 2.36 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Fibrous, Crusts, Massive
- Cleavage
- Perfect On {010}, Good On {110}
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Arid Oxidation Zones of Copper Sulfide Deposits
- Typical price
- $15-100 per specimen depending on crystal quality
Where rockhounds find kröhnkite
Classic worldwide localities
- Chuquicamata Mine, Chile
- Calama, Chile
- Alcaparrosa Mine, Chile
- Copiapo, Chile
Field-hunting tip
Look in arid oxidation zones of copper sulfide deposits country — that is the host setting where kröhnkite typically forms. If you start seeing chalcanthite, brochantite, atacamite in float, you are in the right ground. Field specimens usually show a tabular crystals, fibrous, crusts, massive habit, so train your eye for that shape before scanning the outcrop.





