Kaolinite is a soft, earthy, white clay mineral that is usually found in massive or clay-like aggregates. It is formed primarily through the chemical weathering or hydrothermal alteration of aluminum-silicate minerals like feldspar. Collectors often seek out specimens associated with other minerals in pockets or clay-filled voids.
Is this kaolinite?
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 kaolinite with a known reference. Kaolinite 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 to dull earthy.
- 4Match the color rangeCompare against the expected color range: white, brownish white, grayish white, yellowish white, grayish green.
- 5Look at form & habitCrystal system: triclinic. Typical habit: earthy.
Often confused with
Kaolinite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kaolinite
Minerals reported to co-occur with kaolinite. 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
- 2.61-2.68 g/cm³
- Streak
- White
- Luster
- Pearly to dull earthy
- Transparency
- Transparent to translucent as single crystals
- Crystal system
- Triclinic
- Crystal habit
- Earthy
- Cleavage
- Perfect on {001}
- Rarity
- Common
- Uses
- Industrial, Ceramics, Paper filler, Cosmetics, Collector
- Host rock
- Replaces other aluminosilicate minerals during hydrothermal alteration and weathering
Where rockhounds find kaolinite
1 mapped spotsClassic worldwide localities
- Macon, Bibb Co., Georgia, USA
- Dixie Clay Company mine, and in the Lamar Pit, near Bath, Aikin Co., South Carolina, USA
- Webster, Jackson Co., North Carolina, USA
- Murfreesboro, Pike Co., and at Greenwood, Sebastian Co., Arkansas, USA
- Kauling, Kiangsi Province, China
- Limoges, Haute-Vienne, France
Field-hunting tip
Where it forms: Replaces other aluminosilicate minerals during hydrothermal alteration and weathering. If you start seeing quartz, feldspar, muscovite 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 Utah. Start trip planning there.






