Gaylussite is a relatively soft, hydrated sodium calcium carbonate mineral typically found in evaporite lake deposits. It is known for its distinctive wedge-shaped, monoclinic crystal habit and its tendency to dehydrate into powdery white coatings if not kept in a stable environment.
Is this gaylussite?
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 gaylussite with a known reference. Gaylussite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Gaylussite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Gaylussite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, gray, yellowish.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: wedge-shaped or prismatic crystals, sometimes elongated.
Often confused with
Gaylussite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside gaylussite
Minerals reported to co-occur with gaylussite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Ca(CO₃)₂·5H₂O
- Mohs hardness
- 2.5-3
- Density
- 1.99 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Wedge-shaped or Prismatic Crystals, Sometimes Elongated
- Cleavage
- Perfect On {110}
- Fluorescence
- Bright White or Yellow Under LW UV
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Evaporite Deposits in Saline Lake Beds
- Typical price
- $10-50 per specimen
Where rockhounds find gaylussite
Classic worldwide localities
- Lake Natron, Tanzania
- Searles Lake, California, USA
- Laguna del Rey, Mexico
- Green River Formation, Wyoming, USA
Field-hunting tip
Look in evaporite deposits in saline lake beds country — that is the host setting where gaylussite typically forms. If you start seeing trona, nahcolite, halite in float, you are in the right ground. Field specimens usually show a wedge-shaped or prismatic crystals, sometimes elongated habit, so train your eye for that shape before scanning the outcrop.





