Yttrocrasite-(Y) is a rare yttrium-rich titano-niobate mineral that typically occurs as massive, opaque black grains. It is primarily found within granite pegmatites and is highly valued by radioactive mineral collectors due to its complex chemical composition and scarcity.
Is this yttrocrasite-(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 yttrocrasite-(y) with a known reference. Yttrocrasite-(Y) sits at Mohs 5.5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: reddish brown.
- 3Read the lusterHold the specimen under a strong light. Luster: bright pitchy to resinous.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: metamict.
Often confused with
Yttrocrasite-(Y) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside yttrocrasite-(y)
Minerals reported to co-occur with yttrocrasite-(y). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Y,Th,Ca,U)(Ti,Fe)₂(O,OH)₆
- Mohs hardness
- 5.5-6
- Density
- 4.80 g/cm³
- Colors
- Streak
- Reddish brown
- Luster
- Bright pitchy to resinous
- Transparency
- Opaque, transparent in thin fragments
- Crystal system
- Orthorhombic
- Crystal habit
- Metamict
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In granite pegmatite
Where rockhounds find yttrocrasite-(y)
Classic worldwide localities
- Burnet Co., Texas, about five km east of Baringer Hill, USA
Field-hunting tip
Where it forms: In granite pegmatite. If you start seeing allanite, quartz, microcline in float, you are in the right ground. Typical habit: metamict. Train your eye for that shape before scanning the outcrop.





