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The supermarket job was challenging and I was given the responsibility that most graduates yearn for: A stream has a natural tendency to reach a base level. Finer sediment carried by the flood is spread farther away from the channel before it is finally deposited. Because its velocity is low, it has lost its ability to erode downward. And a loss of depth. If the rocks in the region are more susceptible to erosion, rockslides and other types of landslides gradually modify the steep slopes to form a V-shaped valley. If it were steeper than needed to transport the sediments erosion would result.
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The second part is the fine-grained material such as clay and silt that is suspended in the water as the stream flows along. SW Samantha Wheeler Oct 27, JR Jayson Rayford Jul 12, Yet streams and rivers are able to create both erosional landforms their own channels, canyons, and valleys and depositional landforms floodplains, alluvial fans, and deltas as they flow over Earth's surface. Harvard University Press,
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The dams have also reduced the amount of natural floods along the river and the velocity of the river's flow. A fast-moving stream carries more sediment and larger material than a slow-moving one. This is known as the bed load. Try to see everyone on the same level--that is, a level deserving of respect and maturity. Reword it in terms of what you can do about it:
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A stream has a natural tendency to reach a base level. This increases the gradient which causes the water to flow faster which increases erosion and transport, which then reduces the gradient. Edit Send to Editors Promote Share to Kinja Toggle Conversation tools Go to permalink. Jet streams, the fast upper-air winds that travel west-to-east around the planet, meander. If the rocks in the region are more susceptible to erosion, rockslides and other types of landslides gradually modify the steep slopes to form a V-shaped valley. The bottom is the stream bed. Because its velocity is low, it has lost its ability to erode downward.
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