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Sand is a naturally occurring granular material composed of finely divided rock and mineral particles. It is defined by size, being finer than gravel and coarser than silt . Sand can also refer to a textural class of soil or soil type; i.e. a soil containing more than 85% sand-sized particles (by mass).

The composition of sand varies, depending on the local rock sources and conditions, but the most common constituent of sand in inland continental settings and non- tropical coastal settings is silica (silicon dioxide, or SiO 2 ), usually in the form of quartz . The second most common type of sand is calcium carbonate , for example aragonite , which has mostly been created, over the past half billion years, by various forms of life, like coral and shellfish . It is, for example, the primary form of sand appa

In terms of particle size as used by geologists , sand particles range in diameter from 0.0625   mm (or 1 ⁄ 16   mm) to 2   mm. An individual particle in this range size is termed a sand grain . Sand grains are between gravel (with particles ranging from 2   mm up to 64   mm) and silt (particles smaller than 0.0625   mm down to 0.004   mm). The size specification between sand and gravel has remained constant for more than a century, but particle diameters as small as 0.02   mm were considered sand under the