Yttrotantalite-(Y) is a rare yttrium-tantalum-niobium oxide mineral often found as dark, brownish-black prismatic crystals in pegmatites. It is notable for its heavy density and characteristic radioactive nature, requiring careful handling by collectors. It is typically sought after by mineralogists interested in rare-earth element bearing species.
Is this yttrotantalite-(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 yttrotantalite-(y) with a known reference. Yttrotantalite-(Y) sits at Mohs 5-5.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Yttrotantalite-(Y) leaves a light brown streak.
- 3Read the lusterHold the specimen under a strong light. Yttrotantalite-(Y) typically shows a resinous luster.
- 4Match the color rangeCompare against the expected color range: black, brown, yellowish-brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic crystals, flattened or wedge-shaped.
Often confused with
Yttrotantalite-(Y) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside yttrotantalite-(y)
Minerals reported to co-occur with yttrotantalite-(y). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Y,U,Fe)(Ta,Nb)O₄
- Mohs hardness
- 5-5.5
- Density
- 5.5-6.7 g/cm³
- Streak
- Light Brown
- Luster
- Resinous
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic Crystals, Flattened or Wedge-shaped
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- $50-500 thumbnail to cabinet size
Where rockhounds find yttrotantalite-(y)
Classic worldwide localities
- Ytterby, Sweden
- Moss, Norway
- Karelia, Russia
- Western Australia
Field-hunting tip
Look in granite pegmatites country — that is the host setting where yttrotantalite-(y) typically forms. If you start seeing beryl, monazite, zircon in float, you are in the right ground. Field specimens usually show a prismatic crystals, flattened or wedge-shaped habit, so train your eye for that shape before scanning the outcrop.





