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, 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.





