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 1.5-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale blue.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: blue, dark blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: crystalline, encrustations, platy.
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
- 1.5-3
- Density
- 3.32 g/cm³
- Streak
- Pale blue
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Crystalline, encrustations, platy
- Cleavage
- Perfect
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- A secondary mineral formed in the oxidized zone of copper-bearing hydrothermal mineral deposits, commonly of post-mine origin; may occur in slags
Where rockhounds find posnjakite
Classic worldwide localities
- Yellow Pine mine, Crisman, Boulder Co., Colorado, and at the Majuba Hill mine, Antelope district, Pershing Co., Nevada, USA
- Nura-Taldy tungsten deposits, central Kazakhstan
- Cornwall, as at the Drakewalls mine, Gunnislake, and the Fowey Consols mine, Tywardreath, England
- Penrhiw mine, Ystumtuen, Dyfed, Wales
- Muckross mine, Co. Kerry, Ireland
- Salsigne mine, 15 km north of Carcassone, Aude, France
Field-hunting tip
Where it forms: A secondary mineral formed in the oxidized zone of copper-bearing hydrothermal mineral deposits, commonly of post-mine origin; may occur in slags. If you start seeing brochantite, langite, devilline in float, you are in the right ground. Typical habit: crystalline, encrustations, platy. Train your eye for that shape before scanning the outcrop.






