Keckite is a rare phosphate mineral typically found as brown to yellowish-brown fibrous aggregates or crusts. It primarily occurs as a secondary alteration product of primary phosphate minerals within complex granite pegmatites.
Is this keckite?
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 keckite with a known reference. Keckite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Keckite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Keckite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellowish-brown, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous, radiating, or crusts.
Often confused with
Keckite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside keckite
Minerals reported to co-occur with keckite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaMn²⁺₄Fe³⁺₂(PO₄)₄(OH)₄·2H₂O
- Mohs hardness
- 3-4
- Density
- 3.37 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous, Radiating, Or Crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find keckite
Classic worldwide localities
- Hagendorf-Pleystein pegmatite, Bavaria, Germany
- Mangualde pegmatite, Portugal
Field-hunting tip
Look in granite pegmatites country — that is the host setting where keckite typically forms. If you start seeing triphylite, hureaulite, leucophosphite in float, you are in the right ground. Field specimens usually show a fibrous, radiating, or crusts habit, so train your eye for that shape before scanning the outcrop.






