Sand forms the largest particles found in soil. Most sands are quartz with a few other minerals mixed in. Regular sand contains close to an even distribution of grain sizes. Each grain is large enough to be detected individually by touch and easily distinguished by viewing with the naked eye. Sands may be further subdivided into coarse, fine and very fine, according to the material's grittiness, representative percentage of grain sizes and overall feel.
Silt is soil material that contains 80 percent or more of silt and less than 12 percent clay. Silt particles are much smaller than grains of sand but are still largely composed of quartz. Clay particles, the smallest component found in soil, are plate-like in shape and contain a greater amount of nutrients than either silt or sand. Clay gives soil a sticky feel when moistened and can be made into firm casts that harden when dried.
The United States Department of Agriculture sub-classifies the loamy sands from coarse to very fine, according to the proportion of sand separates they contain. Loamy coarse sand contains at least 25 percent of separates that are either very coarse or coarse and less than 50 percent of any other texture. Loamy sand consists of less than 50 percent of fine or very fine particles, more than 25 percent of medium particles, and less than 25 percent of the two coarsest particle types.
Loamy fine sand contains 50 percent or more of fine sand, or less than 50 percent very fine sand in combination with less than 25 percent very coarse, coarse, and medium sand. Loamy very fine sand contains 50 percent or more of very fine sand. This soil is smooth to the touch due to the predominance of excessively fine grains. All types of loamy sands differ from sandy loams as loamy sands contain more silt separates and fewer particles of sand and clay.