Mccrillisite is an extremely rare phosphate mineral known primarily from the Mount Mica pegmatite in Maine. It typically forms as small, tabular crystals associated with other phosphate minerals in complex pegmatitic environments.
Is this mccrillisite?
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 mccrillisite with a known reference. Mccrillisite sits at Mohs 4-4.5, 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: tetragonal. Typical habit: crystalline.
Often confused with
Mccrillisite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside mccrillisite
Minerals reported to co-occur with mccrillisite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCsBeZr₂(PO₄)₄·1-2H₂O
- Mohs hardness
- 4-4.5
- Density
- 3.125 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent to transparent
- Crystal system
- Tetragonal
- Crystal habit
- Crystalline
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare product of late-stage hydrothermal alteration of primary zirconium-bearing minerals, in a complex granite pegmatite
Where rockhounds find mccrillisite
Classic worldwide localities
- Mt. Mica, near Paris, Oxford Co., Maine, USA
Field-hunting tip
Where it forms: A rare product of late-stage hydrothermal alteration of primary zirconium-bearing minerals, in a complex granite pegmatite. If you start seeing zircon, kosnarite, roscherite in float, you are in the right ground. Typical habit: crystalline. Train your eye for that shape before scanning the outcrop.







