Arrojadite-(BaNa) is a rare phosphate mineral predominantly found in granitic pegmatites. It typically appears as dark green to olive-green massive or granular aggregates that can be difficult to distinguish from other phosphate minerals without chemical analysis.
Is this arrojadite-(bana)?
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 arrojadite-(bana) with a known reference. Arrojadite-(BaNa) sits at Mohs 4-5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Arrojadite-(BaNa) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Arrojadite-(BaNa) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: dark green, brownish-green, olive-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: granular to massive.
Often confused with
Arrojadite-(BaNa) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside arrojadite-(bana)
Minerals reported to co-occur with arrojadite-(bana). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Ba(Fe²⁺,Mn²⁺)₁₃Al(PO₄)₁₁(OH,F)₂
- Mohs hardness
- 4-5
- Density
- 3.55 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Granular to Massive
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find arrojadite-(bana)
Classic worldwide localities
- Tip Top Mine, South Dakota, USA
- Mangualde, Portugal
- Buranga pegmatite, Rwanda
- Kola Peninsula, Russia
Field-hunting tip
Look in granite pegmatites country — that is the host setting where arrojadite-(bana) typically forms. If you start seeing albite, quartz, muscovite in float, you are in the right ground. Field specimens usually show a granular to massive habit, so train your eye for that shape before scanning the outcrop.







