Manganolangbeinite is a rare sulfate mineral that forms tetrahedral crystals within volcanic fumarole environments or potash-rich evaporite sequences. It is distinguished from other langbeinite group members by its distinct pink coloration caused by the substitution of manganese into the crystal structure.
Is this manganolangbeinite?
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 manganolangbeinite with a known reference. Manganolangbeinite sits at Mohs 3.5-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Manganolangbeinite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Manganolangbeinite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pink, pale pink, colorless.
- 5Look at form & habitCrystal system: cubic. Typical habit: tetrahedral crystals, granular.
Often confused with
Manganolangbeinite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside manganolangbeinite
Minerals reported to co-occur with manganolangbeinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂Mn₂(SO₄)₃
- Mohs hardness
- 3.5-4
- Density
- 2.83 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Tetrahedral Crystals, Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarole Deposits, Evaporite Deposits
- Typical price
- $20-150 thumbnail
Where rockhounds find manganolangbeinite
Classic worldwide localities
- Vesuvio volcano, Italy
- Caracoles, Chile
Field-hunting tip
Look in fumarole deposits, evaporite deposits country, the host setting where manganolangbeinite typically forms. If you start seeing thenardite, anhydrite, sylvite in float, you are in the right ground. Field specimens usually show a tetrahedral crystals, granular habit, so train your eye for that shape before scanning the outcrop.






