Strontioruizite is an extremely rare strontium-dominant silicate mineral primarily found in hydrothermal vein deposits. It typically forms small, prismatic orange to brown crystals and is of interest primarily to advanced systematic mineral collectors due to its rarity.
Is this strontioruizite?
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 strontioruizite with a known reference. Strontioruizite sits at Mohs 5-5.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: very light brown.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: orange, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Strontioruizite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside strontioruizite
Minerals reported to co-occur with strontioruizite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Sr₂Mn₂Si₄O₁₁(OH)₄·2H₂O
- Mohs hardness
- 5-5.5
- Density
- 3.20 g/cm³
- Streak
- Very light brown
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals
- Cleavage
- Good on {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- On chemically weathered metamorphosed manganese ore
Where rockhounds find strontioruizite
Classic worldwide localities
- N’Chwaning III mine, Kalahari manganese field, Northern Cape province, South Africa
Field-hunting tip
Where it forms: On chemically weathered metamorphosed manganese ore. If you start seeing sugilite, potassic-magnesio-arfvedsonite, lipuite in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.




