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 — that is 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.





