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, 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.





