Schröckingerite is a rare secondary uranium mineral often found as bright yellow, platy or rosette-like aggregates. It is highly prized by collectors for its brilliant yellow-green fluorescence under ultraviolet light. It typically occurs as an efflorescence in oxidized zones of uranium deposits.
Is this schröckingerite?
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 schröckingerite with a known reference. Schröckingerite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Schröckingerite leaves a pale yellow streak.
- 3Read the lusterHold the specimen under a strong light. Schröckingerite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, greenish yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals, rosettes, globular aggregates, crusts.
Often confused with
Schröckingerite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside schröckingerite
Minerals reported to co-occur with schröckingerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCa₃(UO₂)(CO₃)₃(SO₄)F·10H₂O
- Mohs hardness
- 2.5
- Density
- 2.5 g/cm³
- Colors
- Streak
- Pale Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Platy Crystals, Rosettes, Globular Aggregates, Crusts
- Cleavage
- Perfect Basal
- Fluorescence
- Bright Yellowish-green Under UV Light
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Oxidized Uranium Deposits, Hydrothermal Veins
- Typical price
- $20-150 for thumbnail to small cabinet specimens
Where rockhounds find schröckingerite
Classic worldwide localities
- Jachymov, Czech Republic
- Wamsutter, Wyoming, USA
- Marysvale, Utah, USA
- Schneeberg, Germany
Field-hunting tip
Look in oxidized uranium deposits, hydrothermal veins country — that is the host setting where schröckingerite typically forms. If you start seeing uraninite, gypsum, liebigite in float, you are in the right ground. Field specimens usually show a platy crystals, rosettes, globular aggregates, crusts habit, so train your eye for that shape before scanning the outcrop.





