Julienite is a very rare cobalt thiocyanate mineral characterized by its distinct blue-green color and platy, micaceous habit. It is primarily found as crusts or small aggregates in oxidized copper-cobalt mines and is highly prized by advanced mineral collectors due to its unique chemical composition and scarcity.
Is this julienite?
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 julienite with a known reference. Julienite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Julienite leaves a pale blue streak.
- 3Read the lusterHold the specimen under a strong light. Julienite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: blue, blue-green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals, crusts, radial aggregates.
Often confused with
Julienite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside julienite
Minerals reported to co-occur with julienite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Co(NCS)₄·8H₂O
- Mohs hardness
- 2
- Density
- 2.4 g/cm³
- Colors
- Streak
- Pale Blue
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy Crystals, Crusts, Radial Aggregates
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Copper-cobalt Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find julienite
Classic worldwide localities
- Kamoto mine, Democratic Republic of the Congo
Field-hunting tip
Look in oxidized zones of copper-cobalt deposits country — that is the host setting where julienite typically forms. If you start seeing heterogenite, malachite, sphaerocobaltite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts, radial aggregates habit, so train your eye for that shape before scanning the outcrop.




