Manganberzeliite is a rare manganese-dominant member of the garnet supergroup typically found in the famous manganese mines of Sweden. It usually occurs as compact, brownish-yellow granular masses or small dodecahedral crystals associated with various manganese oxides. Its distinct chemistry and rarity make it a prized specimen for advanced systematic mineral collectors.
Is this manganberzeliite?
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 manganberzeliite with a known reference. Manganberzeliite sits at Mohs 5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Manganberzeliite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Manganberzeliite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brownish yellow, orange.
- 5Look at form & habitCrystal system: cubic. Typical habit: dodecahedral crystals, massive, granular.
Often confused with
Manganberzeliite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside manganberzeliite
Minerals reported to co-occur with manganberzeliite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCa₂(Mg₂Mn³⁺₂)As₃O₁₂
- Mohs hardness
- 5
- Density
- 4.15 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Dodecahedral Crystals, Massive, Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Manganese Ore Deposits
- Typical price
- $50-300 per thumbnail specimen
Where rockhounds find manganberzeliite
Classic worldwide localities
- Långban, Sweden
- Jakobsberg, Sweden
Field-hunting tip
Look in metamorphosed manganese ore deposits country — that is the host setting where manganberzeliite typically forms. If you start seeing hausmannite, jacobsite, dolomite in float, you are in the right ground. Field specimens usually show a dodecahedral crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.





