Kamotoite-(Y) is a rare hydrated yttrium uranium uranyl carbonate mineral found in oxidized uranium deposits. It typically forms thin, bright yellow platy crystals or coatings and is highly prized by advanced mineral collectors for its complexity and rarity.
Is this kamotoite-(y)?
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 kamotoite-(y) with a known reference. Kamotoite-(Y) sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kamotoite-(Y) leaves a pale yellow streak.
- 3Read the lusterHold the specimen under a strong light. Kamotoite-(Y) typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, bright yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, tabular aggregates.
Often confused with
Kamotoite-(Y) vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Luster reads pearly on Kamotoite-(Y) and vitreous on Uranophane.

How to tell apart: Kasolite is the harder of the two (Mohs 4-5 vs. 2-3); streak differs — Kamotoite-(Y) leaves pale yellow, Kasolite leaves yellow; luster reads pearly on Kamotoite-(Y) and greasy on Kasolite.
Often found alongside kamotoite-(y)
Minerals reported to co-occur with kamotoite-(y). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Y₂U₄(UO₂)₄(CO₃)₃O₄(OH)₂·14H₂O
- Mohs hardness
- 2-3
- Density
- 4.26 g/cm³
- Colors
- Streak
- Pale Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Tabular Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zone of Uranium-rich Copper-cobalt Deposits
- Typical price
- $50-500 thumbnail size specimen
Where rockhounds find kamotoite-(y)
Classic worldwide localities
- Kamoto-East open-pit mine, Democratic Republic of the Congo
Field-hunting tip
Look in oxidized zone of uranium-rich copper-cobalt deposits country — that is the host setting where kamotoite-(y) typically forms. If you start seeing uraninite, becquerelite, schuilingite-(nd) in float, you are in the right ground. Field specimens usually show a platy crystals, tabular aggregates habit, so train your eye for that shape before scanning the outcrop.



