Carnallite is a soft, deliquescent halide mineral primarily found in marine evaporite deposits. It often appears as massive or granular aggregates that dissolve easily in water and should be stored in a dry environment to prevent degradation.
Is this carnallite?
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 carnallite with a known reference. Carnallite sits at Mohs 2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: greasy, shining.
- 4Match the color rangeCompare against the expected color range: white, blue, colorless, yellow, red.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: fibrous, massive, pseudo hexagonal.
Often confused with
Carnallite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside carnallite
Minerals reported to co-occur with carnallite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KMgCl₃·6H₂O
- Mohs hardness
- 2.5
- Density
- 1.602 g/cm³
- Streak
- White
- Luster
- Greasy, shining
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Fibrous, massive, pseudo hexagonal
- Cleavage
- None
- Rarity
- Common
- Uses
- Industrial, Collector
- Host rock
- Thought to form in saline marine deposits by reaction of pre-existing saline minerals with fluids high in potash
Where rockhounds find carnallite
4 mapped spotsClassic worldwide localities
- Permian salt basin of southeastern New Mexico, in the Carlsbad potash district, Eddy Co., and adjacent parts, Texas, USA
- Paradox basin, Grand Co., Utah, USA
- Leopoldshall and Westeregeln, near Stassfurt, Magdeburg district, Germany
- Kalusz, Ukraine
- Maman, Azerbaijan
- Barcelona and Lerida Provinces, Spain
Field-hunting tip
Where it forms: Thought to form in saline marine deposits by reaction of pre-existing saline minerals with fluids high in potash. If you start seeing kieserite, sylvite, halite in float, you are in the right ground. Typical habit: fibrous, massive, pseudo hexagonal. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Utah, Nevada. Start trip planning there.





