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, 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.






