bed load, a large load
Fast moving. sediment is heavy it settle out in slow water. But a river that just became slow after being fast looks like it has the most, because of all the settling going on.
Factors that affect a river's ability to erode and carry sediment include velocity of the water flow, volume of water, slope of the riverbed, geology of the surrounding area, and the presence of vegetation or obstructions along the river's path. High velocity and volume of water, steep slopes, soft rock formations, and minimal vegetation can increase erosion and sediment transport capacity.
The total quantity of sediment carried by a river is called its sediment load. This includes both suspended sediment (particles floating in the water) and bedload (particles rolling or sliding along the riverbed).
Sediment in a river can move via traction, where particles are pushed or dragged along the riverbed by the flow of water. Saltation involves the bouncing or hopping of smaller sediment particles along the riverbed. Finally, suspension occurs when finer sediment particles are carried within the flowing water column.
The dropping of soil and rocks by rivers is called sediment deposition. As rivers flow, they carry sediment downstream, which can accumulate and settle along the riverbed or on the floodplain. This process helps in shaping the landscape and forming features like river deltas.
sediment
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.
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.
The smaller the load a river has the more sediment it can carry is false. When the river has more energy, it is able to carry a larger load, therefore more sediment.
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 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.
Mature rivers carry large amounts of sediment along their lengths. This helps to shape the land and produce fertile farm lands.
Fast moving water can carry more sediment. Firstly because the potential of erosion rises with flow speed; secondly because larger grains can be transported by faster water and thirdly because the volume flow per unit time increases with flow speed. The actual amount / concentration of sediment transported by a stream is very dependent on the geology of the catchment, i.e. the amount of soft sediment available for erosion.
Fast moving. sediment is heavy it settle out in slow water. But a river that just became slow after being fast looks like it has the most, because of all the settling going on.