Johnsomervilleite is a very rare phosphate mineral typically occurring as tiny, granular masses in phosphate-rich concretions. It is best known from the unique mineral localities of the Big Fish River area in Yukon, Canada, where it forms alongside other secondary phosphate minerals.
Is this johnsomervilleite?
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 johnsomervilleite with a known reference. Johnsomervilleite sits at Mohs 4-5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Johnsomervilleite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Johnsomervilleite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, pinkish-brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: granular.
Often confused with
Johnsomervilleite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside johnsomervilleite
Minerals reported to co-occur with johnsomervilleite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂CaMg₃Fe²⁺₂(PO₄)₄
- Mohs hardness
- 4-5
- Density
- 3.55 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Granular
- Cleavage
- None Observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Phosphate-rich Sedimentary Concretions
- Typical price
- $50-250 for rare micro-mounts
Where rockhounds find johnsomervilleite
Classic worldwide localities
- Big Fish River, Yukon, Canada
- Rapid Creek, Yukon, Canada
Field-hunting tip
Look in phosphate-rich sedimentary concretions country — that is the host setting where johnsomervilleite typically forms. If you start seeing gormanite, ludlamite, satterlyite in float, you are in the right ground. Field specimens usually show a granular habit, so train your eye for that shape before scanning the outcrop.





