Table of Contents
- 1 What happens when a stream reaches base level?
- 2 What is a stream’s base level?
- 3 What are two consequences of raising the base level of a stream by building a dam?
- 4 What happens to a stream’s base level when a reservoir is constructed?
- 5 What can change base level?
- 6 Why does gradient decrease downstream?
- 7 How does the gradient of a stream affect how much erosion it causes?
- 8 What affects stream velocity?
What happens when a stream reaches base level?
At the location where a stream reaches its base level, it slows down and deposits nearly all of the sediment it is carrying. A stream that comes down a canyon and enters a flat valley or plain builds a fan shaped deposit of sediment known as an alluvial fan. Alluvial fans are built mostly during flash floods.
What is a stream’s base level?
baselevel, in hydrology and geomorphology, limit below which a stream cannot erode. Upon entering a still body of water, a stream’s velocity is checked and thus it loses its eroding power; hence, the approximate level of the surface of the still water body is the stream’s baselevel.
Why does base level fall increase stream power?
At the base level, the water in the stream has less velocity, which means the water flow has less energy, so its ability to erode or chip away at the land surrounding it is decreased.
What are two consequences of raising the base level of a stream by building a dam?
Dams alter habitat Gravel, logs, and other important food and habitat features can also become trapped behind dams. This negatively affects the creation and maintenance of more complex habitat (e.g., riffles, pools) downstream.
What happens to a stream’s base level when a reservoir is constructed?
What happens to a local base level when a reservoir is constructed? A local, or temporary, base level may control a regional landscape and the lower limit of local streams. That local base level might be a river, a lake, a hard and resistant rock structure, or a human-made dam.
What does base level control?
In geology and geomorphology a base level is the lower limit for an erosion process. The height of a base level also influences the position of deltas and river terraces. Together with river discharge and sediment flux the position of the base level influences the gradient, width and bed conditions in rivers.
What can change base level?
Base level change may be related to the following factors: Sea level change. Tectonic movement. River capture. Extensive sedimentation.
Why does gradient decrease downstream?
Gradient (the slope of the land) decreases as rivers flow because the river meanders across the land rather than erode into it and follow a straight path as it does in the source. This means it covers a decrease in height over a longer distance the further downstream you get.
What factors would decrease flow velocity?
1, water flow velocity is decreased by friction along the stream bed, so it is slowest at the bottom and edges and fastest near the surface and in the middle. In fact, the velocity just below the surface is typically a little higher than right at the surface because of friction between the water and the air.
How does the gradient of a stream affect how much erosion it causes?
If the slope is too gentle and velocity is too slow to transport the sediments being supplied by weathering and erosion, the sediments will pile up. This increases the gradient which causes the water to flow faster which increases erosion and transport, which then reduces the gradient.
What affects stream velocity?
The velocity of a river is determined by many factors, including the shape of its channel, the gradient of the slope that the river moves along, the volume of water that the river carries and the amount of friction caused by rough edges within the riverbed.
How does gradient affect the velocity of a stream?
Streams that carry larger particles have greater competence. Streams with a steep gradient (slope) have a faster velocity and greater competence. Particles that are too large to be carried as suspended loads are bumped and pushed along the stream bed, called bed load.