Yoshimuraite is a rare barium-manganese titanium silicate mineral typically found in metamorphic manganese deposits. Collectors should look for its distinctive yellow-brown tabular or bladed crystals associated with other manganese minerals like rhodochrosite.
Is this yoshimuraite?
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 yoshimuraite with a known reference. Yoshimuraite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Yoshimuraite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Yoshimuraite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, yellow-brown.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, bladed, lamellar aggregates.
Often confused with
Yoshimuraite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside yoshimuraite
Minerals reported to co-occur with yoshimuraite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ba₂Mn₂Ti(Si₂O₇)(PO₄)(OH,Cl)
- Mohs hardness
- 3-4
- Density
- 3.84 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Bladed, Lamellar Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Manganese Ore Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find yoshimuraite
Classic worldwide localities
- Tanohata Mine, Japan
- Noda-Tamagawa Mine, Japan
Field-hunting tip
Look in metamorphosed manganese ore deposits country — that is the host setting where yoshimuraite typically forms. If you start seeing manganophyllite, rhodochrosite, bustamite in float, you are in the right ground. Field specimens usually show a tabular crystals, bladed, lamellar aggregates habit, so train your eye for that shape before scanning the outcrop.





