Canasite is a rare phyllosilicate mineral typically found in unique alkaline environments like the Kola Peninsula. It is best identified by its distinct bladed or fibrous habit and its characteristic bright yellow fluorescence under short-wave UV light.
Is this canasite?
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 canasite with a known reference. Canasite 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: brownish yellow, green yellow, light green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: bladed, massive, or fibrous aggregates.
Often confused with
Canasite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside canasite
Minerals reported to co-occur with canasite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₃Na₃Ca₅Si₁₂O₃₀(OH)₄
- Mohs hardness
- 5-6
- Density
- 2.707 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Bladed, massive, or fibrous aggregates
- Cleavage
- One, very perfect; another, perfect, at 118° to the first
- Fluorescence
- Bright yellow under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In pegmatites in a differentiated alkalic massif (Khibiny massif, Russia); in charoitic rocks (Murun massif, Russia)
Where rockhounds find canasite
Classic worldwide localities
- Mts. Yukspor and Rasvumchorr, Khibiny massif, Kola Peninsula, and in the Murun massif, southwest of Olekminsk, Yakutia, Russia
Field-hunting tip
Where it forms: In pegmatites in a differentiated alkalic massif (Khibiny massif, Russia); in charoitic rocks (Murun massif, Russia). If you start seeing fenaksite, lamprophyllite, titanite in float, you are in the right ground. Typical habit: bladed, massive, or fibrous aggregates. Train your eye for that shape before scanning the outcrop.









