Yttrocolumbite-(Y) is a rare yttrium-rich niobium-tantalum oxide found primarily in complex granitic pegmatites. It typically appears as dark, resinous, massive material and is often radioactive due to the presence of uranium within its crystal structure.
Is this yttrocolumbite-(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 yttrocolumbite-(y) with a known reference. Yttrocolumbite-(Y) sits at Mohs 5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: brown.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: massive, tabular crystals, or crusts.
Often confused with
Yttrocolumbite-(Y) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside yttrocolumbite-(y)
Minerals reported to co-occur with yttrocolumbite-(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)₂(Nb,Ta)₂O₆
- Mohs hardness
- 5
- Density
- 5.49 g/cm³
- Colors
- Streak
- Brown
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Massive, tabular crystals, or crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare accessory mineral in granite pegmatites
Where rockhounds find yttrocolumbite-(y)
Classic worldwide localities
- Mozambique (type locality)
Field-hunting tip
Where it forms: A rare accessory mineral in granite pegmatites. If you start seeing feldspar, quartz, mica in float, you are in the right ground. Typical habit: massive, tabular crystals, or crusts. Train your eye for that shape before scanning the outcrop.






