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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to earthy, waxy.
- 4Match the color rangeCompare against the expected color range: white, green, blue, yellow, brown.
- 5Look at form & habitCrystal system: amorphous. Typical habit: botryoidal, encrustations, stalactitic.
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
- 2.75 g/cm³
- Streak
- White
- Luster
- Vitreous to earthy, waxy
- Transparency
- Translucent
- Crystal system
- Amorphous
- Crystal habit
- Botryoidal, encrustations, stalactitic
- Cleavage
- None
- Fluorescence
- Blue under SW UV
- Rarity
- Common
- Uses
- Collector, Scientific research
- Host rock
- A weathering product of volcanic ash
Where rockhounds find allophane
2 mapped spotsClassic worldwide localities
- Bisbee, and the Maid of Sunshine mine, Gleeson, Cochise Co., Arizona, USA
- Kelly, Socorro Co., New Mexico, USA
- Cerro Gordo, Inyo Co., California, USA
- Friedensville, Lehigh Co. and Cornwall, Lebanon Co., Pennsylvania, USA
- Gräfenthal, near Saalfeld, Thuringia, and at Schneeberg and Schwarzenberg, Saxony, Germany
- Jáchymov (Joachimsthal), Czech Republic
Field-hunting tip
Where it forms: A weathering product of volcanic ash. If you start seeing quartz, cristobalite, imogolite in float, you are in the right ground. Typical habit: botryoidal, encrustations, stalactitic. 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.







