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 — that is 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.






