Povondraite is a rare member of the tourmaline group, typically forming as fine, acicular needles or dark, fibrous mats. Collectors primarily prize it for its unique iron-rich composition and its relative scarcity in well-crystallized form compared to common black schorl.
Is this povondraite?
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 povondraite with a known reference. Povondraite 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. Povondraite leaves a brownish black streak.
- 3Read the lusterHold the specimen under a strong light. Povondraite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: black, dark brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: acicular needles, radiating fibrous aggregates.
Often confused with
Povondraite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside povondraite
Minerals reported to co-occur with povondraite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaFe³⁺₃(Fe³⁺₄Mg₂)Si₆O₁₈(BO₃)₃(OH)₃O
- Mohs hardness
- 6.5-7
- Density
- 3.36 g/cm³
- Colors
- Streak
- Brownish Black
- Luster
- Vitreous
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Acicular Needles, Radiating Fibrous Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Hydrothermal Veins in Granitic Pegmatites
- Typical price
- $50-500 depending on specimen quality and rarity
Where rockhounds find povondraite
Classic worldwide localities
- San Piero in Campo, Elba, Italy
- Alto Chaparral, California, USA
- Magnet Cove, Arkansas, USA
Field-hunting tip
Look in hydrothermal veins in granitic pegmatites country — that is the host setting where povondraite typically forms. If you start seeing quartz, albite, microcline in float, you are in the right ground. Field specimens usually show a acicular needles, radiating fibrous aggregates habit, so train your eye for that shape before scanning the outcrop.





