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.

Hardness
2-2.5
Mohs
Luster
Dull
Streak
White
Transparency
Opaque

Is this kaolinite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try 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.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Kaolinite leaves a white streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Kaolinite typically shows a dull luster.
  • 4
    Match the color range
    Compare against the expected color range: white, grayish, yellowish, brownish.
  • 5
    Look at form & habit
    Crystal system: triclinic. Typical habit: massive.

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
2.6-2.68 g/cm³
Streak
White
Luster
Dull
Transparency
Opaque
Crystal system
Triclinic
Crystal habit
Massive
Cleavage
Perfect Basal
Rarity
Common
Uses
Industrial, Ceramics, Paper Filler, Cosmetics, Collector
Host rock
Hydrothermal Alteration Zones and Sedimentary Clay Deposits
Typical price
$5-20 for study specimens

Where rockhounds find kaolinite

1 mapped spots

Classic worldwide localities

  • China
  • USA (Georgia)
  • France
  • United Kingdom (Cornwall)
  • Czech Republic

Field-hunting tip

Look in hydrothermal alteration zones and sedimentary clay deposits country — that is the host setting where kaolinite typically forms. If you start seeing quartz, feldspar, muscovite in float, you are in the right ground. Field specimens usually show a massive habit, so 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.

Common questions

How do you identify kaolinite?+
Mohs hardness is 2-2.5. It typically shows a dull luster. The streak is white. Common colors include white, grayish, yellowish, brownish.
Where is kaolinite found?+
Notable localities include China; USA (Georgia); France; United Kingdom (Cornwall); Czech Republic.
Can I find kaolinite in the United States?+
RockHoundR maps 1 kaolinite rockhounding spots across 1 U.S. states — the top states are Utah.
How much is kaolinite worth?+
Typical asking prices fall in the range of $5-20 for study specimens. Quality, size, and provenance can move individual specimens well outside that range.
What rocks look like kaolinite?+
Kaolinite is most often confused with Talc, Pyrophyllite, Montmorillonite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with kaolinite?+
Kaolinite commonly co-occurs with Quartz, Feldspar, Muscovite, Tourmaline. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does kaolinite form in?+
Kaolinite typically forms in hydrothermal alteration zones and sedimentary clay deposits. Working float back to the host body is the standard way to chase a fresh occurrence.
What is kaolinite used for?+
Kaolinite is used in industrial, ceramics, paper filler, cosmetics, collector.

Find kaolinite on the map

RockHoundR shows mapped rockhounding spots, access rules, and lets you log every find.

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