Dewindtite is a secondary uranium phosphate mineral that typically forms as bright yellow, thin platy crystals or powdery crusts. It is most commonly found in the oxidized zones of uranium-rich hydrothermal deposits where lead is present. Due to its high radioactivity and toxicity, it is strictly a specimen for experienced collectors who follow proper safety protocols.
Is this dewindtite?
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 dewindtite with a known reference. Dewindtite sits at Mohs 2.5-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: pearly.
- 4Match the color rangeCompare against the expected color range: greenish yellow, yellow, light yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: pulverulent, striated, tabular.
Often confused with
Dewindtite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Luster reads pearly on Dewindtite and vitreous, pearly on {001} on Autunite.

How to tell apart: Luster reads pearly on Dewindtite and vitreous, subadamantine, waxy, pearly on cleavages; becoming dull on dehydration to metatorbernite on Torbernite.

How to tell apart: Streak differs, so Dewindtite leaves pale yellow, Phosphuranylite leaves light yellow; luster reads pearly on Dewindtite and vitreous to pearly on Phosphuranylite.
Often found alongside dewindtite
Minerals reported to co-occur with dewindtite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₃(UO₂)₆(PO₄)₄O₂(OH)₂·12H₂O
- Mohs hardness
- 2.5-3
- Density
- 5.03 g/cm³
- Streak
- Pale yellow
- Luster
- Pearly
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Pulverulent, striated, tabular
- Cleavage
- {100}, perfect
- Fluorescence
- Green under SW and LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral formed by alteration of uraninite or earlier-formed secondary uranium minerals
Where rockhounds find dewindtite
Classic worldwide localities
- Shinkolobwe and Swambo, Katanga Province, Congo (Shaba Province, Zaire)
- Wölsendorf, Bavaria, and on the Streuberg, near Bergen, and at Schneeberg, Saxony, Germany
- La Faye, near Grury, Saône-et-Loire, and at Kerségalec-en-Lignol, Morbihan, France
- Jáchymov (Joachimsthal), Czech Republic
- Urgeiriça, Portugal
- Takwa and Lac Indicateur areas, Quebec, Canada
Field-hunting tip
Where it forms: A rare secondary mineral formed by alteration of uraninite or earlier-formed secondary uranium minerals. If you start seeing torbernite, parsonsite, dumontite in float, you are in the right ground. Typical habit: pulverulent, striated, tabular. Train your eye for that shape before scanning the outcrop.




