clay.
load
The total sediment load transported by a stream is the sum of the bed load, suspended load, and dissolved load. Bed load consists of larger particles that roll, slide, and bounce along the streambed. Suspended load is finer particles carried in the water column, while dissolved load is material that is dissolved in the water itself.
Due to long shore currents the suspended particles transported as a suspended load to the deep sea.
Suspended load refers to sediment particles carried within the water column of a stream, while bed load refers to sediment particles that are transported along the streambed through rolling, sliding, or saltation. Suspended load typically consists of smaller particles that remain suspended in the water, while bed load consists of larger particles that move along the streambed.
It is called suspension.
Suspended load refers to sediment particles carried in the water column, while bed load refers to sediment particles that are transported along the riverbed through rolling, sliding, or saltating movements. Suspended load is typically finer particles that remain suspended in the water, while bed load is larger particles that move along the riverbed.
Stream transport sediment in three ways, dissolved load, (ions in solution being carried downstream), suspended load, (suspended sediment that floats freely downstream) and bed load, (sediment that rolls or scoots along the bottom of the river).
A suspended load.
The difference between a suspended load and a bead load is a suspended load consists of the small particles or rock materials that are dispersed throughout the water and easily carried downstream. The bead load consists of the larger particles that are dragged and bounced along near the bottom of the river.
bed load. This type of stream load consists of heavier materials that are transported along the stream bed through rolling, sliding, or bouncing. It tends to move more slowly than suspended load or dissolved load.
Geologists commonly us the term STREAM for any body of water that flows in a channel.TOTAL LOADRivers move not only water but also a tremendous amount of material. This material, called the total load, consists of bed load, suspended load and dissolved load. Bed loadcomprises particles of sand and gravel that slide, roll, and bounce along the channel bottom in rapidly moving water. Suspended load comprises mainly silt and clay particles carried in suspension above the riverbed. Dissolved load comprises electrically charged atoms or molecules, called ions, that are carried in solution in the water
Bed load is a term used in the field of geomorphology to describe the particles such as sand, gravel, and pebbles that are transported along the bed of a river or stream by rolling, sliding, or bouncing. These particles are too heavy to be suspended in the water column, unlike suspended load. Bed load movement can contribute to erosion and sediment transport in river systems.