Clay is a finely-grained natural
soil material that combines one or more
clay minerals with possible traces of
metal oxides and
organic matter. Geologic clay
deposits are mostly composed of
phyllosilicate minerals containing variable amounts of
water trapped in the mineral structure. Clays are
plastic due to particle size and geometry as well as water content and become hard, brittle and non–plastic upon drying or
Depending on the soil's content in which it is found, clay can appear in various colours from white to dull grey or brown to deep orange-red.
Electron microscope photograph of smectite clay – magnification 23,500
Although many naturally occurring deposits include both silts and clay, clays are distinguished from other fine-grained soils by differences in size and mineralogy.
Silts, which are fine-grained soils that do not include clay minerals, tend to have larger particle sizes than clays. There is, however, some overlap in particle size and other physical properties. The distinction between silt and clay varies by discipline.
soil scientists usually consider the separation to occur at a particle size of 2
µm (clays being finer than silts),
sedimentologists often use 4–5 μm, and
chemists use 1 μm.
Geotechnical engineers distinguish between silts and clays based on the plasticity properties of the soil, as measured by the soils'
Atterberg limits. ISO 14688 grades clay particles as being smaller than 2 μm and silt particles as being larger.
silt and less than 40% clay are called
loam. Loam makes good
soil and is used as a building material.