Tobelite is a rare ammonium-bearing mica that commonly forms in low-temperature hydrothermal environments associated with organic-rich sediments. It is often visually indistinguishable from muscovite or illite, requiring X-ray diffraction or chemical analysis for positive identification.
Is this tobelite?
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 tobelite with a known reference. Tobelite sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Tobelite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Tobelite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, grayish.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy aggregates, scaly masses.
Often confused with
Tobelite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside tobelite
Minerals reported to co-occur with tobelite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (NH₄)Al₂(Si₃Al)O₁₀(OH)₂
- Mohs hardness
- 2-3
- Density
- 2.7-2.8 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Aggregates, Scaly Masses
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Clay Deposits, Coal-bearing Sedimentary Rocks
- Typical price
- $20-100 per specimen
Where rockhounds find tobelite
Classic worldwide localities
- Toba, Japan
- Coal measures, Czech Republic
Field-hunting tip
Look in hydrothermal clay deposits, coal-bearing sedimentary rocks country — that is the host setting where tobelite typically forms. If you start seeing quartz, kaolinite, pyrophyllite in float, you are in the right ground. Field specimens usually show a platy aggregates, scaly masses habit, so train your eye for that shape before scanning the outcrop.






