Halloysite is a clay mineral frequently found as an alteration product of aluminosilicate minerals. It is best identified by its distinct tubular micro-structure and earthy texture, which sets it apart from other kaolinite-group minerals in fine detail.
Is this halloysite?
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 halloysite with a known reference. Halloysite sits at Mohs 2-2.5, 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: pearly, waxy, or dull.
- 4Match the color rangeCompare against the expected color range: white, yellowish white, reddish white, brownish white, greenish white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: earthy.
Often confused with
Halloysite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside halloysite
Minerals reported to co-occur with halloysite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Al₂Si₂O₅(OH)₄
- Mohs hardness
- 2-2.5
- Density
- 2.55-2.565 g/cm³
- Streak
- White
- Luster
- Pearly, waxy, or dull
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Earthy
- Cleavage
- {001}, probable
- Rarity
- Common
- Uses
- Ceramics, Industrial absorbent, Catalyst carrier
- Host rock
- A product of hydrothermal alteration or surface weathering of aluminosilicate minerals, as feldspars
Where rockhounds find halloysite
5 mapped spotsClassic worldwide localities
- Wagon Wheel Gap, Mineral Co., Colorado, USA
- Gonzales, Gonzales Co., Texas, USA
- Bedford, Lawrence Co., Indiana, USA
- Horse Cove, Hart Co., Kentucky, USA
- Bergnersreuth, near Wunsiedel, Bavaria, Germany
Field-hunting tip
Where it forms: A product of hydrothermal alteration or surface weathering of aluminosilicate minerals, as feldspars. If you start seeing kaolinite, endellite, allophane in float, you are in the right ground. Typical habit: earthy. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Georgia, Colorado, North Carolina. Start trip planning there.






