Childrenite is an iron-rich phosphate mineral often found in complex granite pegmatites. It typically forms attractive, honey-brown to reddish-brown prismatic crystals that are highly sought after by systematic mineral collectors.
Is this childrenite?
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 childrenite with a known reference. Childrenite sits at Mohs 5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to resinous.
- 4Match the color rangeCompare against the expected color range: white, yellowish brown, brownish black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy, prismatic, tabular.
Often confused with
Childrenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside childrenite
Minerals reported to co-occur with childrenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeAlPO₄(OH)₂·H₂O
- Mohs hardness
- 5
- Density
- 3.11-3.19 g/cm³
- Streak
- White
- Luster
- Vitreous to resinous
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy, prismatic, tabular
- Cleavage
- {100}, poor
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- In some complex granite pegmatites, typically a low-temperature hydrothermal alteration product of primary phosphate minerals
Where rockhounds find childrenite
1 mapped spotsClassic worldwide localities
- Palermo #1 mine, near North Groton, Grafton Co., New Hampshire, USA
- Devon, near Tavistock, at Wheal Crebor, the George and Charlotte mine, Russell United mines, Wheal Betsy, England
- Cornwall, in the Crinnis and Carlyon mine, Wheal Jane, England
- Cobalt mine, Scar Crag, Causey Pike, Keswick, Cumbria, England
- Greifensteine, near Ehrenfriedersdorf, Saxony, and Hagendorf, Bavaria
- Stari Trg mine (Trepča), Kosovo, Serbia
Field-hunting tip
Where it forms: In some complex granite pegmatites, typically a low-temperature hydrothermal alteration product of primary phosphate minerals. If you start seeing siderite, pyrite, apatite in float, you are in the right ground. Typical habit: platy, prismatic, tabular. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in New Hampshire. Start trip planning there.









