Allophane is an amorphous, poorly ordered aluminosilicate mineral typically found as a secondary product in weathered volcanic soils or hydrothermal deposits. It is best identified by its clay-like, waxy appearance and tendency to occur in botryoidal or earthy masses, often requiring XRD analysis for positive confirmation.
Is this allophane?
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 allophane with a known reference. Allophane sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Allophane leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Allophane typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, blue, green, yellow, brown, colorless.
- 5Look at form & habitCrystal system: amorphous. Typical habit: earthy, massive, encrusting, botryoidal.
Often confused with
Allophane vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside allophane
Minerals reported to co-occur with allophane. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Al₂O₃·(SiO₂)₁₋₂·nH₂O
- Mohs hardness
- 3
- Density
- 1.8-2.0 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Amorphous
- Crystal habit
- Earthy, Massive, Encrusting, Botryoidal
- Cleavage
- None
- Rarity
- Common
- Uses
- Collector, Scientific Research
- Host rock
- Weathered Volcanic Ash, Hydrothermal Alteration Zones
- Typical price
- $10-50 for small samples
Where rockhounds find allophane
2 mapped spotsClassic worldwide localities
- Japan
- Germany
- New Zealand
- USA
- Russia
Field-hunting tip
Look in weathered volcanic ash, hydrothermal alteration zones country, the host setting where allophane typically forms. If you start seeing gibbsite, kaolinite, halloysite in float, you are in the right ground. Field specimens usually show a earthy, massive, encrusting, botryoidal habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Colorado, Missouri. Start trip planning there.







