Magnesio-foitite is a rare member of the tourmaline group defined by a vacancy in the X-site of its crystal structure. Collectors typically find it as small, pale bluish gray or violet prismatic crystals embedded in pegmatite matrices. It is physically similar to other tourmalines and often requires chemical analysis for definitive identification.
Is this magnesio-foitite?
3-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 magnesio-foitite with a known reference. Magnesio-foitite sits at Mohs ~7, softer than the next harder reference, harder than the previous one.
- 2Match the color rangeCompare against the expected color range: pale bluish gray.
- 3Look at form & habitCrystal system: trigonal. Typical habit: prismatic crystals.
Often confused with
Magnesio-foitite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside magnesio-foitite
Minerals reported to co-occur with magnesio-foitite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- ☐(Mg₂Al)Al₆Si₆O₁₈(BO₃)₃(OH)₄
- Mohs hardness
- ~7
- Density
- 2.995 g/cm³
- Colors
- Pale bluish gray
- Transparency
- Transparent to translucent
- Crystal system
- Trigonal
- Crystal habit
- Prismatic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- From an alteration zone in a silicified porphyry developed in completely altered andesitic to dacitic volcanic rocks (Japan); in unconformity-type uranium deposits (Canada)
Where rockhounds find magnesio-foitite
Classic worldwide localities
- Kyonosawa, Mitomi-mura, Higashi-Yamanashi-gun, Yamanashi-ken Prefecture, Honshu, ~100 km west of Tokyo, Japan
- Rabbit Lake and Second Link Lake, eastern edge of the Athabasca Basin, Saskatchewan, Canada
Field-hunting tip
Where it forms: From an alteration zone in a silicified porphyry developed in completely altered andesitic to dacitic volcanic rocks (Japan); in unconformity-type uranium deposits (Canada). If you start seeing hematite, pyrite, rutile in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.








