Szymańskiite is an extremely rare mercury-bearing phosphate mineral typically found as delicate, acicular, white-to-colorless crystal sprays. It is primarily known from the Kidd Creek mine in Ontario, where it occurs in hydrothermal environments. Due to its rarity and mercury content, it is strictly a specimen for advanced mineral collectors.
Is this szymańskiite?
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 szymańskiite with a known reference. Szymańskiite sits at Mohs 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Szymańskiite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Szymańskiite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: acicular crystals, radiated aggregates.
Often confused with
Szymańskiite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside szymańskiite
Minerals reported to co-occur with szymańskiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Hg⁺(H₃O)₂Al₂(PO₄)₂(OH)₂·2H₂O
- Mohs hardness
- 3
- Density
- 2.44 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Acicular Crystals, Radiated Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Mines
- Typical price
- expensive; rare micro-specimen pricing
Where rockhounds find szymańskiite
Classic worldwide localities
- Kidd Creek mine, Ontario, Canada
Field-hunting tip
Look in hydrothermal veins in mines country — that is the host setting where szymańskiite typically forms. If you start seeing quartz, albite, dolomite in float, you are in the right ground. Field specimens usually show a acicular crystals, radiated aggregates habit, so train your eye for that shape before scanning the outcrop.





