Posnjakite is a secondary copper sulfate mineral that forms beautiful, vibrant blue, platy crystal clusters. It is often found as a crust or coating in the oxidized zones of copper mines and is frequently associated with other copper minerals like brochantite and langite.
Is this posnjakite?
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 posnjakite with a known reference. Posnjakite sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Posnjakite leaves a pale blue streak.
- 3Read the lusterHold the specimen under a strong light. Posnjakite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: blue, greenish-blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, crusts, rosettes, radiating aggregates.
Often confused with
Posnjakite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside posnjakite
Minerals reported to co-occur with posnjakite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₄(SO₄)(OH)₆·H₂O
- Mohs hardness
- 2-3
- Density
- 3.84 g/cm³
- Colors
- Streak
- Pale Blue
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Crusts, Rosettes, Radiating Aggregates
- Cleavage
- Perfect in One Direction
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Oxidized Zones of Copper-rich Sulfide Deposits
- Typical price
- $10-60 for small specimens
Where rockhounds find posnjakite
Classic worldwide localities
- Kastelorizo, Greece
- Bisbee, Arizona, USA
- Cornwall, England
- Schneeberg, Germany
- Mina Profunda, Chile
Field-hunting tip
Look in oxidized zones of copper-rich sulfide deposits country — that is the host setting where posnjakite typically forms. If you start seeing brochantite, langite, chalcopyrite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts, rosettes, radiating aggregates habit, so train your eye for that shape before scanning the outcrop.






