Proto-ferro-suenoite is a rare member of the amphibole supergroup that was formally defined based on specific cation arrangements in the crystal lattice. It typically occurs as small prismatic crystals in high-grade metamorphic environments, often associated with manganese-rich mineral suites.
Is this proto-ferro-suenoite?
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 proto-ferro-suenoite with a known reference. Proto-ferro-suenoite sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Proto-ferro-suenoite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Proto-ferro-suenoite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brownish-yellow, pale brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Proto-ferro-suenoite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside proto-ferro-suenoite
Minerals reported to co-occur with proto-ferro-suenoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- □Mn₂Mg₅Si₈O₂₂(OH)₂
- Mohs hardness
- 5-6
- Density
- 3.35-3.45 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals
- Cleavage
- Perfect On {110}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find proto-ferro-suenoite
Classic worldwide localities
- Kyauk-Pyat-That, Mogok, Myanmar
Field-hunting tip
Look in metamorphic rocks country — that is the host setting where proto-ferro-suenoite typically forms. If you start seeing spessartine, rhodonite, calcite in float, you are in the right ground. Field specimens usually show a prismatic crystals habit, so train your eye for that shape before scanning the outcrop.






