Löweite is a rare sodium-magnesium sulfate mineral found primarily in marine salt deposits. It typically forms as colorless to yellowish tabular crystals or massive aggregates within evaporite sequences.
Is this löweite?
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 löweite with a known reference. Löweite 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, gray, pale yellow, reddish yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, massive, granular.
Often confused with
Löweite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside löweite
Minerals reported to co-occur with löweite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₁₂Mg₇(SO₄)₁₃·15H₂O
- Mohs hardness
- 2.5-3
- Density
- 2.36-2.42 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Tabular crystals, massive, granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- An uncommon mineral in marine salt deposits; in efflorescences and crusts in saline playa deposits; a volcanic sublimation product
Where rockhounds find löweite
Classic worldwide localities
- Carlsbad potash district, Eddy Co., New Mexico, USA
- Northwest of Grand Junction, Mesa Co., Colorado, USA
- Ischl, Hallstatt, and Hall, Austria
- Stassfurt-Aschersleben-Bernburg potash district, Saxony-Anhalt, Germany
- Merkers, Thuringia, Germany
- Hattorf, near Philippsthal, and at Neuhof-Ellers, Hesse, Germany
Field-hunting tip
Where it forms: An uncommon mineral in marine salt deposits; in efflorescences and crusts in saline playa deposits; a volcanic sublimation product. If you start seeing anhydrite, gypsum, vanthoffite in float, you are in the right ground. Typical habit: tabular crystals, massive, granular. Train your eye for that shape before scanning the outcrop.








