as slope increases erosion rate increases (direct relationship)
As flood waters rise, the slope of the stream as it flows to it's base level increases
The slope or gradient of the stream is the most likely factor to affect the amount of erosion. Steeper slopes result in higher velocities, which in turn increase the erosive power of the stream. A steeper slope also allows the stream to carry larger sediment and potentially cause more erosion.
other soils have a poor resistance to erosion. A slope can increase the affects of erosion, obviously, because it increases speed, and destruction of the runoff and sediment.
If a rivers slope decreases, its ability to erode land under it decreases too. The slope determines the rivers velocity. The steeper the slope, the higher the velocity, the more erosion.
A steep slope increases the water flow, and the erosion wherever the bank is formed from softer material than rock, can be quite great when the river is in flood. Deposition is increased when the flow slows in the lower reaches as the river reaches the valley, and the gravel and silt is able to settle.
Erosion increases due to the effective gravitational gradient.
As flood waters rise, the slope of the stream as it flows to it's base level increases
true
The slope or gradient of the stream is the most likely factor to affect the amount of erosion. Steeper slopes result in higher velocities, which in turn increase the erosive power of the stream. A steeper slope also allows the stream to carry larger sediment and potentially cause more erosion.
Things that would cause a stream to move faster would be how large the stream is, how much material is in the stream and how much of a slope the stream is at. Things blocking the stream would also cause it to move slower.
erosion deposition weathering and a lot more...
It simply means that when one variable increases, the other increases as well.
other soils have a poor resistance to erosion. A slope can increase the affects of erosion, obviously, because it increases speed, and destruction of the runoff and sediment.
Changing the slope of the stream table affects the speed and direction of water flow. A steeper slope creates faster water flow, which can result in more erosion and deposition. Conversely, a flatter slope slows down water flow, leading to less erosion and deposition. These changes in flow dynamics can cause differences in the shape and size of channels, as well as the amount and distribution of sediment carried by the water.
If the slope is negative, y decreases as x increases. The slope goes from top-left of the graph (Quadrant II) to the lower-right of the graph (Quadrant IV).
If a rivers slope decreases, its ability to erode land under it decreases too. The slope determines the rivers velocity. The steeper the slope, the higher the velocity, the more erosion.
A steep slope increases the water flow, and the erosion wherever the bank is formed from softer material than rock, can be quite great when the river is in flood. Deposition is increased when the flow slows in the lower reaches as the river reaches the valley, and the gravel and silt is able to settle.