Imogolite is a rare aluminosilicate clay mineral that typically forms as extremely fine, hollow nanotubes in volcanic soils. It is rarely found in macroscopic crystals and is primarily studied for its unique nanostructure and high surface area in geological and materials science.
Is this imogolite?
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 imogolite with a known reference. Imogolite 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous, resinous, waxy.
- 4Match the color rangeCompare against the expected color range: yellowish white, light brownish yellow, blue, green, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: earthy.
Often confused with
Imogolite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside imogolite
Minerals reported to co-occur with imogolite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Al₂SiO₃(OH)₄
- Mohs hardness
- 2-3
- Density
- 2.70 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous, resinous, waxy
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Earthy
- Cleavage
- None
- Rarity
- Uncommon
- Uses
- Scientific research, Catalysis
- Host rock
- In soils derived from volcanic ash
Where rockhounds find imogolite
Classic worldwide localities
- Misutsuchi bed, Iijima, Nagano Prefecture, Japan
- Kanumatsuchi bed, Kanuma, Tochigi Prefecture, Japan
- Uemura, Kumamoto Prefecture, Japan
Field-hunting tip
Where it forms: In soils derived from volcanic ash. If you start seeing allophane, quartz, cristobalite in float, you are in the right ground. Typical habit: earthy. Train your eye for that shape before scanning the outcrop.







