Mangani-pargasite is a rare member of the amphibole supergroup characterized by significant manganese substitution. It typically occurs as dark prismatic crystals within metamorphosed carbonate rocks and is primarily sought after by advanced collectors of manganese-rich mineral suites.
Is this mangani-pargasite?
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 mangani-pargasite with a known reference. Mangani-pargasite 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. Mangani-pargasite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Mangani-pargasite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: dark green, black, brownish-black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Mangani-pargasite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside mangani-pargasite
Minerals reported to co-occur with mangani-pargasite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCa₂ (Mg₄Mn) (Al₂Si₆O₂₂) (OH)₂
- Mohs hardness
- 5-6
- Density
- 3.2-3.4 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals
- Cleavage
- Perfect in Two Directions
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Limestone
- Typical price
- $20-200 per specimen
Where rockhounds find mangani-pargasite
Classic worldwide localities
- Långban, Sweden
- Franklin, New Jersey, USA
Field-hunting tip
Look in metamorphosed limestone country — that is the host setting where mangani-pargasite typically forms. If you start seeing calcite, dolomite, willemite 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.








