Pyroxmangite is a rare manganese silicate that is easily confused with the more common rhodonite. It is typically found in manganese-rich metamorphic deposits, often appearing as pinkish-brown to red granular masses or small, flattened crystals.
Is this pyroxmangite?
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 pyroxmangite with a known reference. Pyroxmangite sits at Mohs 5.5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Pyroxmangite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pyroxmangite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pink, reddish-brown, brown, yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, massive, granular.
Often confused with
Pyroxmangite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside pyroxmangite
Minerals reported to co-occur with pyroxmangite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MnSiO₃
- Mohs hardness
- 5.5-6
- Density
- 3.6-3.8 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Perfect in Two Directions
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Manganese-rich Metamorphic Rocks
- Typical price
- $20-150 for small specimens
Where rockhounds find pyroxmangite
Classic worldwide localities
- South Carolina, USA
- Valle di Scalve, Italy
- Broken Hill, Australia
- Hokkaido, Japan
- Tanzania
Field-hunting tip
Look in manganese-rich metamorphic rocks country — that is the host setting where pyroxmangite typically forms. If you start seeing rhodonite, spessartine, quartz in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.






