Sudoite is a di-trioctahedral chlorite mineral, historically referred to as an Al-rich chlorite or dioctahedral-trioctahedral chlorite. Collectors typically find it as white or gray micaceous scales or platy aggregates often associated with alteration zones in volcanic rocks.
Is this sudoite?
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 sudoite with a known reference. Sudoite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Sudoite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Sudoite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, gray, greenish.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, micaceous masses, scaly aggregates.
Often confused with
Sudoite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside sudoite
Minerals reported to co-occur with sudoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₂(Al,Fe³⁺,Mg)₃(Si₃Al)O₁₀(OH)₈
- Mohs hardness
- 2.5-3
- Density
- 2.5-2.7 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Micaceous Masses, Scaly Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Hydrothermal Veins, Metamorphic Rocks, Weathered Volcanic Rocks
- Typical price
- $10-50 per specimen
Where rockhounds find sudoite
Classic worldwide localities
- Sudo, Japan
- Belledonne Massif, France
- Kola Peninsula, Russia
- Hartz Mountains, Germany
Field-hunting tip
Look in hydrothermal veins, metamorphic rocks, weathered volcanic rocks country — that is the host setting where sudoite typically forms. If you start seeing quartz, pyrite, kaolinite in float, you are in the right ground. Field specimens usually show a platy crystals, micaceous masses, scaly aggregates habit, so train your eye for that shape before scanning the outcrop.






