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 — that is 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.







