Struvite-(K) is a rare phosphate mineral occurring in environments rich in organic matter and phosphates. Collectors typically encounter it as small, fragile, tabular to wedge-shaped crystals that are highly sensitive to dehydration. Proper storage in a cool, sealed container is essential to prevent the crystals from crumbling into powder.
Is this struvite-(k)?
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 struvite-(k) with a known reference. Struvite-(K) 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. Struvite-(K) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Struvite-(K) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellowish-white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, wedge-shaped crystals.
Often confused with
Struvite-(K) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside struvite-(k)
Minerals reported to co-occur with struvite-(k). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KMg(PO₄)·6H₂O
- Mohs hardness
- 2
- Density
- 1.72 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Wedge-shaped Crystals
- Cleavage
- Distinct On {001}
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Phosphate-rich Environments
- Typical price
- $50-300 per specimen
Where rockhounds find struvite-(k)
Classic worldwide localities
- Srednaya Padma mine, Karelia, Russia
- various phosphate-rich guano deposits
Field-hunting tip
Look in phosphate-rich environments country — that is the host setting where struvite-(k) typically forms. If you start seeing struvite, newberyite, variscite in float, you are in the right ground. Field specimens usually show a tabular crystals, wedge-shaped crystals habit, so train your eye for that shape before scanning the outcrop.



