Ashcroftine-(Y) is a rare potassium-sodium-yttrium silicate mineral known for its striking pink, radiating, or needle-like crystal aggregates. It is primarily found in highly alkaline pegmatites, often appearing as delicate, fibrous sprays associated with other rare earth minerals.
Is this ashcroftine-(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 ashcroftine-(y) with a known reference. Ashcroftine-(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, may be silky.
- 4Match the color rangeCompare against the expected color range: pink, light violet, pinkish brown, deep violet.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: fibrous, prismatic.
Often confused with
Ashcroftine-(Y) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ashcroftine-(y)
Minerals reported to co-occur with ashcroftine-(y). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₅Na₅Y₁₂Si₂₈O₇₀(OH)₂(CO₃)₈·8H₂O
- Mohs hardness
- 5
- Density
- 2.61 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous, may be silky
- Transparency
- Transparent to translucent
- Crystal system
- Tetragonal
- Crystal habit
- Fibrous, prismatic
- Cleavage
- Perfect on {100}, distinct on {001}
- Fluorescence
- Bright white/pale yellow under LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In cavities in augite syenite (Narssârssuk, Greenland); in igneous breccia and pegmatites in an intrusive alkalic gabbro-syenite complex (Mont Saint-Hilaire, Canada)
Where rockhounds find ashcroftine-(y)
Classic worldwide localities
- Narssârssuk, Greenland
- Mont Saint-Hilaire, Quebec, Canada
- Cava del 'Osa, near Rome, Lazio, Italy
Field-hunting tip
Where it forms: In cavities in augite syenite (Narssârssuk, Greenland); in igneous breccia and pegmatites in an intrusive alkalic gabbro-syenite complex (Mont Saint-Hilaire, Canada). If you start seeing calcite, elpidite, albite in float, you are in the right ground. Typical habit: fibrous, prismatic. Train your eye for that shape before scanning the outcrop.









