Barrydawsonite-(Y) is an exceptionally rare phosphate mineral belonging to the apatite supergroup. It is typically found as small, inconspicuous grains within the complex alkaline pegmatites of the Khibiny Massif on the Kola Peninsula.
Is this barrydawsonite-(y)?
3-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 barrydawsonite-(y) with a known reference. Barrydawsonite-(Y) sits at Mohs 5, softer than the next harder reference, harder than the previous one.
- 2Match the color rangeCompare against the expected color range: colorless, pale brown.
- 3Look at form & habitCrystal system: monoclinic. Typical habit: anhedral grains and small inclusions.
Often confused with
Barrydawsonite-(Y) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside barrydawsonite-(y)
Minerals reported to co-occur with barrydawsonite-(y). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₁.₅Y₀.₅CaSi₃O₉H
- Mohs hardness
- 5
- Density
- 3.161 g/cm³
- Colors
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Anhedral grains and small inclusions
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Poikilitic in amphibole and pyroxene in metamorphosed eudialyte-syenite
Where rockhounds find barrydawsonite-(y)
Classic worldwide localities
- Merlot Claim, North Red Wine Pluton, Labrador, Canada
Field-hunting tip
Where it forms: Poikilitic in amphibole and pyroxene in metamorphosed eudialyte-syenite. If you start seeing y-bearing pectolite, arfvedsonite, jadeitic aegirine in float, you are in the right ground. Typical habit: anhedral grains and small inclusions. Train your eye for that shape before scanning the outcrop.



