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, 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.




