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  2. The majority of soils may be regarded as either SANDS or CLAYS: SANDS include gravelly sands and gravel-sands. Sand grains are generally broken rock particles that have been formed by physical weathering, or they are the resistant components of rocks broken down by chemical weathering. Sand grains generally have a rotund shape.
    environment.uwe.ac.uk/geocal/SoilMech/classification/default.htm
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