Hydroxycancrinite is a relatively rare silicate mineral that typically forms as an alteration product of nepheline in alkaline igneous environments. It is best identified by its distinct hexagonal crystal structure and strong fluorescence under ultraviolet light, appearing as white to yellowish massive or prismatic aggregates.
Is this hydroxycancrinite?
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 hydroxycancrinite with a known reference. Hydroxycancrinite sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Hydroxycancrinite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Hydroxycancrinite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, gray, yellow, colorless.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: massive, prismatic crystals.
Often confused with
Hydroxycancrinite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside hydroxycancrinite
Minerals reported to co-occur with hydroxycancrinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,Ca)₈(Al₆Si₆O₂₄)(OH,CO₃)₂·nH₂O
- Mohs hardness
- 5-6
- Density
- 2.4-2.5 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Massive, Prismatic Crystals
- Cleavage
- Perfect in One Direction
- Fluorescence
- Bright Yellow or Orange Under UV
- Rarity
- Rare
- Uses
- Collector, Mineralogical Study
- Host rock
- Alkaline Igneous Rocks, Pegmatites
- Typical price
- $20-100 for small specimens
Where rockhounds find hydroxycancrinite
Classic worldwide localities
- Kola Peninsula, Russia
- Mont Saint-Hilaire, Canada
- Langesundsfjord, Norway
Field-hunting tip
Look in alkaline igneous rocks, pegmatites country — that is the host setting where hydroxycancrinite typically forms. If you start seeing nepheline, sodalite, aegirine in float, you are in the right ground. Field specimens usually show a massive, prismatic crystals habit, so train your eye for that shape before scanning the outcrop.





