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 4.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: yellow white.
- 3Read the lusterHold the specimen under a strong light. Luster: dull.
- 4Match the color rangeCompare against the expected color range: brown, gray brown, yellow brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fan shaped.
Often confused with
Keckite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Keckite leaves yellow white, Rockbridgeite leaves greenish gray; luster reads dull on Keckite and vitreous to dull on Rockbridgeite.

How to tell apart: Keckite is noticeably harder (Mohs 4.5 vs. 3.5); streak differs, so Keckite leaves yellow white, Strengite leaves white; luster reads dull on Keckite and vitreous on Strengite.
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
- 4.5
- Density
- 2.60 g/cm³
- Streak
- Yellow white
- Luster
- Dull
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Fan shaped
- Cleavage
- Poor on {001}, and poorer on {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A weathering product of phosphate minerals in a complex granite pegmatite
Where rockhounds find keckite
Classic worldwide localities
- Bavaria, from Hagendorf, at the Silbergrube quarry, near Waidhaus, and at Hühnerkobel, near Zwiesel, Germany
- Bendada pegmatite, near Guarda, Portugal
Field-hunting tip
Where it forms: A weathering product of phosphate minerals in a complex granite pegmatite. If you start seeing rockbridgeite, phosphophyllite, scholzite in float, you are in the right ground. Typical habit: fan shaped. Train your eye for that shape before scanning the outcrop.





