Satpaevite is a rare aluminum vanadium oxide mineral typically occurring as delicate yellow, radiating fibrous or acicular crusts. It is primarily found in the oxidized zones of sandstone-hosted uranium-vanadium deposits, often requiring magnification for clear identification of its crystal form.
Is this satpaevite?
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 satpaevite with a known reference. Satpaevite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Satpaevite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Satpaevite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-orange.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: fibrous, acicular, radiating aggregates.
Often confused with
Satpaevite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside satpaevite
Minerals reported to co-occur with satpaevite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Al₁₂V₆O₃₇·30H₂O
- Mohs hardness
- 2
- Density
- 3.37 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Fibrous, Acicular, Radiating Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sedimentary Sandstone Uranium-vanadium Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find satpaevite
Classic worldwide localities
- Dzhezkazgan, Kazakhstan
- Colorado Plateau, USA
Field-hunting tip
Look in sedimentary sandstone uranium-vanadium deposits country — that is the host setting where satpaevite typically forms. If you start seeing vanadium minerals, calcite, gypsum in float, you are in the right ground. Field specimens usually show a fibrous, acicular, radiating aggregates habit, so train your eye for that shape before scanning the outcrop.




