Kannanite is a rare, magnesium-rich variety of the tourmaline group, primarily recognized by its distinct blue to blue-green color. It typically forms elongated, heavily striated prismatic crystals and is primarily sourced from pegmatite deposits.
Is this kannanite?
4-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 kannanite with a known reference. Kannanite sits at Mohs 6, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 3Match the color rangeCompare against the expected color range: brownish orange, orange.
- 4Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic crystals with striated faces.
Often confused with
Kannanite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kannanite
Minerals reported to co-occur with kannanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄Al₄(MgAl)(VO₄)(SiO₄)₂(Si₃O₁₀)(OH)₆
- Mohs hardness
- 6
- Density
- 3.43 g/cm³
- Colors
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic crystals with striated faces
- Cleavage
- None observed. [Expected to be perfect on {010} by analogy with ardennite
- Rarity
- Rare
- Uses
- Gemstone, Collector
- Host rock
- A product of pumpellyite-actinolite-facies metamorphism of Fe-Mn-ore (quartz, hematite, braunite) in metachert
Where rockhounds find kannanite
Classic worldwide localities
- Kannan Mountain, Ozu district, Ehime Prefecture, Japan
Field-hunting tip
Where it forms: A product of pumpellyite-actinolite-facies metamorphism of Fe-Mn-ore (quartz, hematite, braunite) in metachert. If you start seeing ardennite-, piemontite, hematite in float, you are in the right ground. Typical habit: prismatic crystals with striated faces. Train your eye for that shape before scanning the outcrop.





