Arrojadite-(KFe) is a complex phosphate mineral primarily found in granitic pegmatites. Collectors usually find it as massive, olive-green aggregates rather than well-defined crystals, making accurate identification often reliant on chemical analysis or X-ray diffraction.
Is this arrojadite-(kfe)?
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-(kfe) with a known reference. Arrojadite-(KFe) 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-(KFe) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Arrojadite-(KFe) 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, massive, or as rare tabular to equant crystals.
Often confused with
Arrojadite-(KFe) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside arrojadite-(kfe)
Minerals reported to co-occur with arrojadite-(kfe). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KNa₂Fe²⁺₅Al(PO₄)₆(OH)₂
- Mohs hardness
- 4-5
- Density
- 3.5-3.6 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Granular, Massive, Or as Rare Tabular to Equant Crystals
- Cleavage
- Good in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- $20-100 per specimen
Where rockhounds find arrojadite-(kfe)
Classic worldwide localities
- Sapucaia pegmatite, Brazil
- Norrö, Sweden
- Tip Top mine, USA
- Rapid Creek, Canada
Field-hunting tip
Look in granite pegmatites country — that is the host setting where arrojadite-(kfe) typically forms. If you start seeing quartz, muscovite, albite in float, you are in the right ground. Field specimens usually show a granular, massive, or as rare tabular to equant crystals habit, so train your eye for that shape before scanning the outcrop.





