Juonniite is a very rare phosphate mineral typically found as small, white to colorless bladed crystals within granite pegmatites. It is primarily known from the Viitaniemi pegmatite in Finland, occurring in association with other phosphate species. Due to its extreme rarity, it is almost exclusively sought after by advanced systematic mineral collectors.
Is this juonniite?
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 juonniite with a known reference. Juonniite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Juonniite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Juonniite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: bladed crystals.
Often confused with
Juonniite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside juonniite
Minerals reported to co-occur with juonniite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaMg₂(H₂O)₂(PO₄)₂(OH)₂
- Mohs hardness
- 3-4
- Density
- 2.44 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Bladed Crystals
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- varies due to extreme scarcity, often restricted to research or advanced systematic collections
Where rockhounds find juonniite
Classic worldwide localities
- Viitaniemi pegmatite, Eräjärvi, Orivesi, Finland
Field-hunting tip
Look in granite pegmatites country — that is the host setting where juonniite typically forms. If you start seeing beryl, triphylite, quartz in float, you are in the right ground. Field specimens usually show a bladed crystals habit, so train your eye for that shape before scanning the outcrop.





