Maruyamaite is a very rare potassium-dominant member of the tourmaline group, formally described from specimens in Japan. It typically occurs as small, pale-yellow prisms in highly evolved granitic pegmatites. Collectors value it as a significant species for advanced systematic mineral collections.
Is this maruyamaite?
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 maruyamaite with a known reference. Maruyamaite sits at Mohs 7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Maruyamaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Maruyamaite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pale yellow, yellowish-brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: prismatic crystals.
Often confused with
Maruyamaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside maruyamaite
Minerals reported to co-occur with maruyamaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K(MgLi₂Al₆)(Si₆O₁₈)(BO₃)₃(OH)₃F
- Mohs hardness
- 7
- Density
- 3.2 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Prismatic Crystals
- Cleavage
- Indistinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Pegmatites
- Typical price
- $50-500 depending on specimen size and quality
Where rockhounds find maruyamaite
Classic worldwide localities
- Kuschiyama, Japan
Field-hunting tip
Look in pegmatites country, the host setting where maruyamaite typically forms. If you start seeing quartz, feldspar, mica in float, you are in the right ground. Field specimens usually show a prismatic crystals habit, so train your eye for that shape before scanning the outcrop.






