Caseyite is a rare secondary mineral found in oxidized vanadium-uranium deposits. It typically occurs as small, delicate, yellow platy crystals or thin crusts in sandstone cavities.
Is this caseyite?
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 caseyite with a known reference. Caseyite 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. Caseyite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Caseyite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, brownish-yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals, crusts.
Often confused with
Caseyite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Caseyite is noticeably harder (Mohs 2 vs. approx 1); streak differs — Caseyite leaves yellow, Hewettite leaves brownish red.

How to tell apart: Streak differs — Caseyite leaves yellow, Metahewettite leaves deep red; luster reads pearly on Caseyite and subadamantine on Metahewettite.
Often found alongside caseyite
Minerals reported to co-occur with caseyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₄(Al₄(OH)₈)(V₁₀O₂₈)·14H₂O
- Mohs hardness
- 2
- Density
- 2.47 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Platy Crystals, Crusts
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sandstone Cavities
- Typical price
- $50-300 per specimen
Where rockhounds find caseyite
Classic worldwide localities
- Temple Mountain, Emery County, Utah, USA
Field-hunting tip
Look in sandstone cavities country — that is the host setting where caseyite typically forms. If you start seeing gypsum, hummerite, hewettite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts habit, so train your eye for that shape before scanning the outcrop.


