Mieite-(Y) is an extremely rare yttrium-titanium mineral discovered in Japanese pegmatites. It typically occurs as small, tabular brownish-yellow crystals and is highly sought after by advanced systematic mineral collectors due to its limited distribution.
Is this mieite-(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 mieite-(y) with a known reference. Mieite-(Y) sits at Mohs 6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine.
- 4Match the color rangeCompare against the expected color range: amber-yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals.
Often found alongside mieite-(y)
Minerals reported to co-occur with mieite-(y). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Y₄Ti(SiO₄)₂O[F,(OH)]₆
- Mohs hardness
- 6
- Density
- 4.61 g/cm³
- Colors
- Amber-yellow
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a block of granitic pegmatite collected from a talus slope
Where rockhounds find mieite-(y)
Classic worldwide localities
- Souri Valley, Komono, Mie Prefecture, central Japan
- Reported from El’ozero, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In a block of granitic pegmatite collected from a talus slope. If you start seeing quartz, albite, k-feldspar in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.



