Sulphohalite is a rare sulfate-halide mineral found primarily in arid, high-salinity evaporite environments. Collectors look for its characteristic sharp, dodecahedral crystals often associated with halite and other alkaline salts in dried lake beds.
Is this sulphohalite?
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 sulphohalite with a known reference. Sulphohalite sits at Mohs 3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Sulphohalite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Sulphohalite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellow, pale green.
- 5Look at form & habitCrystal system: isometric. Typical habit: dodecahedral crystals, massive.
Often confused with
Sulphohalite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside sulphohalite
Minerals reported to co-occur with sulphohalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₆(SO₄)₂FCl
- Mohs hardness
- 3.5
- Density
- 2.57 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Isometric
- Crystal habit
- Dodecahedral Crystals, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Evaporite Deposits in Saline Lake Beds
- Typical price
- $20-150 per specimen depending on crystal size and clarity
Where rockhounds find sulphohalite
Classic worldwide localities
- Searles Lake, California, USA
- Salton Sea, California, USA
- Lake Natron, Tanzania
- Kola Peninsula, Russia
Field-hunting tip
Look in evaporite deposits in saline lake beds country, the host setting where sulphohalite typically forms. If you start seeing halite, thenardite, borax in float, you are in the right ground. Field specimens usually show a dodecahedral crystals, massive habit, so train your eye for that shape before scanning the outcrop.





