Manganoblödite is a rare manganese-bearing sulfate mineral belonging to the blödite group. It typically occurs as small prismatic crystals within evaporate sequences and is prized by mineral collectors due to its rarity and specific chemical composition.
Is this manganoblödite?
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 manganoblödite with a known reference. Manganoblödite 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: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, reddish pink in aggregates.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Manganoblödite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside manganoblödite
Minerals reported to co-occur with manganoblödite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Mn(SO₄)₂·4H₂O
- Mohs hardness
- 2.5
- Density
- 2.25 g/cm³
- Colors
- ColorlessReddish pink in aggregates
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Coating the walls of underground mine works, related to post-mining oxidation of primary U deposits of the Colorado Plateau type hosted by sandstones
Where rockhounds find manganoblödite
Classic worldwide localities
- Blue Lizard mine, White Canyon district, San Juan County, Utah, USA and at the Womobi mine, near Thologolong, in northern Victoria, Australia
Field-hunting tip
Where it forms: Coating the walls of underground mine works, related to post-mining oxidation of primary U deposits of the Colorado Plateau type hosted by sandstones. If you start seeing mn-co-ni-bearing blödite, chalcanthite, gypsum in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.








