Fourmarierite is a striking secondary uranium mineral characterized by its vibrant orange-red tabular crystals. It is typically found as an alteration product of uraninite in the oxidized zones of uranium deposits, often occurring in dense, subparallel clusters or crusts.
Is this fourmarierite?
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 fourmarierite with a known reference. Fourmarierite 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. Streak: orange.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine to subadamantine.
- 4Match the color rangeCompare against the expected color range: red, brown, carmine red, pink orange, reddish brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: pseudo hexagonal, tabular.
Often confused with
Fourmarierite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Fourmarierite leaves orange, Becquerelite leaves yellow.


How to tell apart: Streak differs, so Fourmarierite leaves orange, Vandenbrandeite leaves green; luster reads adamantine to subadamantine on Fourmarierite and vitreous on Vandenbrandeite.
Often found alongside fourmarierite
Minerals reported to co-occur with fourmarierite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb(UO₂)₄O₃(OH)₄·4H₂O
- Mohs hardness
- 3-4
- Density
- 6.05 g/cm³
- Colors
- Streak
- Orange
- Luster
- Adamantine to subadamantine
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Pseudo hexagonal, tabular
- Cleavage
- {001}, perfect; {100}, imperfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral formed as an alteration product of uraninite in the oxide zone of uranium deposits; a common component of “gummite” replacing uraninite; may replace fossil wood
Where rockhounds find fourmarierite
Classic worldwide localities
- Palermo mine, near North Groton, Grafton Co., New Hampshire, USA
- Newry, Oxford Co., Maine, USA
- Liepers quarry, Swarthmore, Delaware Co., Pennsylvania, USA
- Spruce Pine, Mitchell Co., North Carolina, USA
- Relatively Shinkolobwe, Katanga Province, Congo (Shaba Province, Zaire)
- Morogoro, Uluguru Mountains, Tanzania
Field-hunting tip
Where it forms: A rare secondary mineral formed as an alteration product of uraninite in the oxide zone of uranium deposits; a common component of “gummite” replacing uraninite; may replace fossil wood. If you start seeing uraninite, ianthinite, schoepite in float, you are in the right ground. Typical habit: pseudo hexagonal, tabular. Train your eye for that shape before scanning the outcrop.




