Foggite is a rare phosphate mineral primarily known from the Big Fish River area in the Yukon. It typically occurs as small, delicate, white to colorless acicular or lath-like crystals associated with other rare secondary phosphates in vugs.
Is this foggite?
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 foggite with a known reference. Foggite 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. Foggite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Foggite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular to lath-like crystals.
Often confused with
Foggite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside foggite
Minerals reported to co-occur with foggite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaAl(PO₄)(OH)₂·H₂O
- Mohs hardness
- 3-4
- Density
- 2.81 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular to Lath-like Crystals
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Phosphate-rich Sedimentary Concretions in Iron Formation
- Typical price
- $50-300 for high-quality micro-specimens
Where rockhounds find foggite
Classic worldwide localities
- Big Fish River, Yukon, Canada
- Rapid Creek, Yukon, Canada
Field-hunting tip
Look in phosphate-rich sedimentary concretions in iron formation country — that is the host setting where foggite typically forms. If you start seeing montgomeryite, englishite, crandallite in float, you are in the right ground. Field specimens usually show a acicular to lath-like crystals habit, so train your eye for that shape before scanning the outcrop.





