Sursassite is a rare manganese aluminum silicate typically found as reddish-brown fibrous or radiating needle-like crystals. It is most commonly identified in manganese-rich metamorphic deposits, often associated with braunite and quartz. Collectors usually seek it out as micro-specimens from its type locality in the Swiss Alps.
Is this sursassite?
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 sursassite with a known reference. Sursassite sits at Mohs 6.5-7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Sursassite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Sursassite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: reddish-brown, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous, radiating aggregates, massive.
Often confused with
Sursassite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside sursassite
Minerals reported to co-occur with sursassite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn²⁺₂Al₃(Si₂O₇)(SiO₄)O(OH)₃
- Mohs hardness
- 6.5-7
- Density
- 3.37 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous, Radiating Aggregates, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Manganiferous Metamorphic Rocks
- Typical price
- $20-150 for thumbnail specimens
Where rockhounds find sursassite
Classic worldwide localities
- Graubünden, Switzerland
- Val d'Err, Switzerland
- Ogliastra, Italy
Field-hunting tip
Look in manganiferous metamorphic rocks country, the host setting where sursassite typically forms. If you start seeing quartz, braunite, tansanite in float, you are in the right ground. Field specimens usually show a fibrous, radiating aggregates, massive habit, so train your eye for that shape before scanning the outcrop.




