Tosudite is a complex interstratified clay mineral composed of chlorite-like and smectite-like layers. It typically forms as a soft, earthy, or platy secondary mineral in hydrothermal alteration zones and is primarily sought after by advanced collectors of clay mineral species.
Is this tosudite?
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 tosudite with a known reference. Tosudite sits at Mohs 1.5-2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Tosudite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Tosudite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, gray, yellow, greenish.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, massive, fine-grained aggregates.
Often confused with
Tosudite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside tosudite
Minerals reported to co-occur with tosudite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₀.₅(Al,Mg)₆(Si,Al)₈O₂₀(OH)₁₀·4H₂O
- Mohs hardness
- 1.5-2
- Density
- 2.3-2.6 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Massive, Fine-grained Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Hydrothermal Veins, Alteration Zones of Clay Deposits
- Typical price
- $20-80 for small cabinet specimens
Where rockhounds find tosudite
Classic worldwide localities
- Tosudo, Japan
- Urals, Russia
- Kazakhstan
- France
Field-hunting tip
Look in hydrothermal veins, alteration zones of clay deposits country, the host setting where tosudite typically forms. If you start seeing quartz, pyrite, kaolinite in float, you are in the right ground. Field specimens usually show a platy crystals, massive, fine-grained aggregates habit, so train your eye for that shape before scanning the outcrop.







