The load of a river is the matter it carries past a cross-section, in three parts that differ by how they travel. The dissolved load is the matter in solution, ions and dissolved silica, which moves with the water at its own speed. The suspended load is made of grains held up within the flow by its turbulence, mostly clay, silt and fine sand, which move at nearly the speed of the water and seldom touch the bed. The bed load is made of grains that roll, slide or hop along the bed, in frequent contact with it, much more slowly than the water.