Innsbruckite is an extremely rare manganese silicate mineral first identified in the Innsbruck region of Austria. It is typically found as small, tabular monoclinic crystals in metamorphic environments and is primarily valued by advanced mineralogists for its scarcity.
Is this innsbruckite?
3-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 innsbruckite with a known reference. Innsbruckite sits at Mohs 6, softer than the next harder reference, harder than the previous one.
- 2Match the color rangeCompare against the expected color range: colorless, white, yellowish.
- 3Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Innsbruckite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside innsbruckite
Minerals reported to co-occur with innsbruckite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn₃₃(Si₂O₅)₁₄(OH)₃₈
- Mohs hardness
- 6
- Density
- 3.216 g/cm³
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Between serpentinite and chert, related to a late hydration stage after blueschist-facies metamorphism of former Mn-rich marine sediments
Where rockhounds find innsbruckite
Classic worldwide localities
- Staffelsee (Geier), Navis valley, 20 km southeast of Innsbruck, Tyrol, Austria
Field-hunting tip
Where it forms: Between serpentinite and chert, related to a late hydration stage after blueschist-facies metamorphism of former Mn-rich marine sediments. If you start seeing rhodochrosite, friedelite, tephroite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.








