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, 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.




