Rinkite-(Y) is a complex sorosilicate mineral found primarily in alkaline igneous rocks. It typically forms colorless to white prismatic crystals and is prized by collectors of rare earth minerals for its association with exotic pegmatite assemblages.
Is this rinkite-(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 rinkite-(y) with a known reference. Rinkite-(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: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Rinkite-(Y) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside rinkite-(y)
Minerals reported to co-occur with rinkite-(y). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Ca₄YTi(Si₂O₇)₂OF₃
- Mohs hardness
- ~5
- Density
- 3.44 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals
- Cleavage
- Very good on {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a pegmatite fragment from an alkaline massif collected from the moraine of the Darai-Pioz glacier
Where rockhounds find rinkite-(y)
Classic worldwide localities
- Darai-Pioz alkaline massif, Tien Shan mountains, Tajikistan
Field-hunting tip
Where it forms: In a pegmatite fragment from an alkaline massif collected from the moraine of the Darai-Pioz glacier. If you start seeing quartz, aegirine, microcline in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.








