Suspended load: All organic and inorganic material carried in moving water Dissolved load: All organic and inorganic material carried in solution by moving water Bed load: Coarse materials such as gravel, stones. These things move along the bottom of the river by rolling, or sliding.
Clay, sand, silt.
I'm pretty sure it is called "deposition".
Stream erode their channels by abrasion, grinding, and by dissolving soluble material. Stream transport sediment in three ways.1. in solution (dissolved load)2. in suspension (suspended load)3. scooting or rolling along the bottom (bed load)Hope that helps. Lot of people trolling this days...Please do not delete.
Shaking ground during an earthquake can cause soft sediment to liquefy due to the increased pore water pressure within the sediment. As the ground shakes, the grains of sediment are rearranged, leading to a reduction in contact between them, which allows water to fill the spaces. This process reduces the sediment's load-bearing capacity, effectively transforming it from a solid state to a fluid-like state, resulting in phenomena such as quicksand or mudflows. Consequently, structures built on such liquefied sediments can experience significant instability and damage.
I don't know what you mean, but I hope this helps: Deposition is the putting down of a load. In geological terms, by a glacier, river, or wind mainly.
The steeper the slope, the faster the water will run, and the more sediment it can carry.The larger the volume of water that is moving, the more sediment it can carry with it.
The steeper the slope, the faster the water will run, and the more sediment it can carry.The larger the volume of water that is moving, the more sediment it can carry with it.
Load quantity in rivers refers to the amount of sediment (such as sand, silt, and gravel) carried by the flowing water. It can be influenced by factors such as erosion, sediment sources, and flow velocity. High load quantities can impact water quality, river ecosystems, and flood risk.
As a river gets older sediment load decreases due to the age of the river and erosion
the amount of sediment a river is carrying during flow
Moving water is a major force in the transport of sediment. The force of water helps to erode, transport, and deposit sediment in various environments like rivers, streams, and coastlines. The energy of moving water can vary depending on factors such as velocity, volume, and sediment load.
Actually, the larger the load a river has, the more sediment it can carry. A river's capacity to transport sediment is often determined by factors like its velocity and volume of water flow. When a river has a larger load, it can transport more sediment downstream.
The amount of sediment a river can carry is primarily controlled by its velocity, water discharge, and the size and density of the sediment particles. Faster-flowing rivers can transport larger and heavier sediments, while slower rivers may only carry finer particles. Additionally, changes in the river's gradient, channel shape, and vegetation along the banks can also influence sediment transport capacity. Erosional processes upstream and sediment deposition downstream further affect the overall sediment load.
load
Sediment derived from the weathering of rocks, and run-off from the land, being washed into the water.
it puts dirt in it making the water dirty :) <3
Most rivers with a large sediment load also have high water velocity because faster-moving water has greater energy, allowing it to transport more sediment. Increased velocity helps lift and carry heavier particles, preventing them from settling. Additionally, steeper gradients and turbulent flow often characterize such rivers, further enhancing their ability to erode and transport sediments. This dynamic relationship between water velocity and sediment load is crucial for shaping river landscapes.