Kaolinite specimen

Crystal & mineral guide

Kaolinite

Al₂Si₂O₅(OH)₄

IndustrialClayMineral

Primary china-clay mineral — ceramics, paper, and industrial filler.

Identify Kaolinite with RockScan

About Kaolinite

Kaolinite is a soft white clay mineral from feldspar weathering. Essential for porcelain (china clay), paper coating, and fillers. Earthy masses lack visible crystals in hand sample. Distinguishes from chalk by silicate chemistry and lack of strong acid fizz.

Kaolinite belongs in a crystal identifier workflow because photo cues — color zoning, crystal habit, and surface luster — combine with measurable traits like Mohs 2–2.5 and specific gravity 2.16–2.68. Use RockScan’s camera to get a first-pass ID, then confirm with the checklist below.

Kaolinite properties

Mohs hardness2–2.5
Crystal systemTriclinic
LusterEarthy to dull
ColorWhite to cream
CompositionAluminum phyllosilicate clay
FormationWeathering of feldspar-rich rocks
OccurrenceChina, USA, UK (Cornwall), Brazil
Specific gravity2.16–2.68
CleavagePerfect basal (micro)

How to identify Kaolinite

  1. Soft white earthy masses
  2. Plastic when wet; earthy odor
  3. Minimal acid reaction vs chalk/calcite

Collector notes

  • Name from Gaoling ('high ridge') hill in China
  • Enabled European porcelain industry after Chinese trade

Value context: Industrial grades by brightness, plasticity, and purity.

Kaolinite FAQ

How do you identify Kaolinite?

Kaolinite (Al₂Si₂O₅(OH)₄) is typically recognized by white to cream color, earthy to dull luster, Mohs hardness 2–2.5, and triclinic crystal system. RockScan can suggest Kaolinite from a photo and surface these checks on the result card.

What is Kaolinite made of?

Kaolinite composition: Aluminum phyllosilicate clay. It forms via weathering of feldspar-rich rocks and is found in China, USA, UK (Cornwall), Brazil.

Is Kaolinite valuable?

Industrial grades by brightness, plasticity, and purity.