Momoiite is a rare manganese-vanadium garnet species first discovered in Japan. It is prized by collectors for its vibrant yellow-green to emerald-green hue, caused by the presence of vanadium, and is typically found in manganese deposits or associated skarn environments.
Is this momoiite?
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 momoiite with a known reference. Momoiite sits at Mohs 7-7.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Momoiite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Momoiite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow-green, emerald-green, yellowish-brown.
- 5Look at form & habitCrystal system: cubic. Typical habit: dodecahedral or trapezohedral crystals.
Often confused with
Momoiite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside momoiite
Minerals reported to co-occur with momoiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mn²⁺,Ca)₃(V³⁺,Al)₂Si₃O₁₂
- Mohs hardness
- 7-7.5
- Density
- 3.75-3.85 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Dodecahedral or Trapezohedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Manganese-rich Metamorphic Rocks and Skarns
- Typical price
- $50-500 per specimen depending on size and intensity of green color
Where rockhounds find momoiite
Classic worldwide localities
- Fujii mine, Japan
- Kuruman district, South Africa
- Tanohata mine, Japan
Field-hunting tip
Look in manganese-rich metamorphic rocks and skarns country — that is the host setting where momoiite typically forms. If you start seeing rhodochrosite, quartz, spessartine in float, you are in the right ground. Field specimens usually show a dodecahedral or trapezohedral crystals habit, so train your eye for that shape before scanning the outcrop.







