How is clay formed?
The result of a long natural process, clay is the result of the gradual weathering, under the influence of climatic phenomena, of rocks containing silicon. Over the years, through erosion and sedimentation, the minerals in the original rock break down, are transported by water and wind, and eventually transform into new clay minerals. This slow metamorphosis takes place differently depending on the parent rock, the original soil and the local climate, which is why there are different varieties of clay (1).
What is its composition?
At a microscopic level, clay appears as a stack of thin layers, much like a mineral mille-feuille. These layers are composed of silicon and aluminium, and sometimes even iron or magnesium, depending on the type of clay. This layered structure enables the clay to retain water and capture impurities, as well as any other substances present on its surface – a quality that is highly sought after in cosmetics (2).
What are the different types of clay?
Clays belong to the phyllosilicate family. There are several types of clay, which can be classified according to their colour:
Green clay: the best known, it comes in two forms, Illite and Montmorillonite. It is rich in silica and magnesium.
White clay : also known as kaolin, it is rich in silica and has a low concentration of mineral salts. Its white colour comes from its high alumina content.
Red clay: it contains a lot of iron oxide, which gives it its colour.
Yellow clay: less well known, it is particularly rich in magnesium and iron.






