Pirssonite is a rare hydrated sodium calcium carbonate mineral that typically forms as sharp, wedge-shaped or tabular crystals in evaporite environments. It is most famous for its occurrence in the alkaline brine deposits of Searles Lake, where it is found associated with other rare carbonates and sulfates. Collectors prize it for its distinct crystal geometry and transparency, though it is prone to dehydration if kept in very dry conditions.
Is this pirssonite?
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 pirssonite with a known reference. Pirssonite sits at Mohs 3-3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Pirssonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pirssonite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellowish.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular to prismatic crystals, often wedge-shaped.
Often confused with
Pirssonite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside pirssonite
Minerals reported to co-occur with pirssonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Ca(CO₃)₂·2H₂O
- Mohs hardness
- 3-3.5
- Density
- 2.35 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular to Prismatic Crystals, Often Wedge-shaped
- Cleavage
- Distinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Evaporite Deposits in Alkaline Lake Beds
- Typical price
- $20-150 per specimen depending on size and quality
Where rockhounds find pirssonite
Classic worldwide localities
- Searles Lake, California, USA
- Olduvai Gorge, Tanzania
- Khibiny Massif, Russia
Field-hunting tip
Look in evaporite deposits in alkaline lake beds country — that is the host setting where pirssonite typically forms. If you start seeing gaylussite, nahcolite, trona in float, you are in the right ground. Field specimens usually show a tabular to prismatic crystals, often wedge-shaped habit, so train your eye for that shape before scanning the outcrop.





