Peatite-(Y) is an extremely rare yttrium carbonate mineral typically found as an alteration product of other yttrium-bearing minerals. Collectors usually identify it by its dull, earthy, or fibrous white crusts forming in cavities or on weathered pegmatite minerals.
Is this peatite-(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 peatite-(y) with a known reference. Peatite-(Y) sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Peatite-(Y) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Peatite-(Y) typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: white, yellowish-white, grayish-white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: fibrous, earthy, massive.
Often confused with
Peatite-(Y) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside peatite-(y)
Minerals reported to co-occur with peatite-(y). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Y₂(CO₃)₃·nH₂O
- Mohs hardness
- 3-4
- Density
- 3.3-3.6 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Fibrous, Earthy, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find peatite-(y)
Classic worldwide localities
- Sweden
- USA
- Norway
- Canada
Field-hunting tip
Look in granite pegmatites country — that is the host setting where peatite-(y) typically forms. If you start seeing allanite, gadolinite, fluorite in float, you are in the right ground. Field specimens usually show a fibrous, earthy, massive habit, so train your eye for that shape before scanning the outcrop.







