Schmitterite is an extremely rare uranium tellurite mineral typically found as a secondary oxidation product. It usually appears as fine-grained, pale yellow crusts or tiny, delicate platy crystals, often associated with other rare tellurium minerals in uranium-rich localities.
Is this schmitterite?
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 schmitterite with a known reference. Schmitterite sits at Mohs 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Schmitterite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Schmitterite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, pale yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals, crusts, pulverulent aggregates.
Often confused with
Schmitterite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside schmitterite
Minerals reported to co-occur with schmitterite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- UO₂TeO₃
- Mohs hardness
- 3
- Density
- 6.05 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy Crystals, Crusts, Pulverulent Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Uranium-tellurium Bearing Hydrothermal Deposits
- Typical price
- $50-300 per thumbnail specimen
Where rockhounds find schmitterite
Classic worldwide localities
- Moab, Utah, USA
- Marysvale, Utah, USA
- Gunnison County, Colorado, USA
Field-hunting tip
Look in oxidized zones of uranium-tellurium bearing hydrothermal deposits country — that is the host setting where schmitterite typically forms. If you start seeing uraninite, tellurium, pyrite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts, pulverulent aggregates habit, so train your eye for that shape before scanning the outcrop.




