The level of the lake
The lowest base level a stream may flow into is sea level in which it flows into the ocean.
The level of a body of water that a stream flows into is called the "base level." It represents the lowest point to which a stream can erode its channel. When a stream reaches its base level, it can no longer lower its bed through erosion, leading to sediment deposition instead. This base level can be influenced by factors such as sea level, dams, or geological uplift.
The base level is the lowest point to which a stream can erode its channel. This can be the level of the body of water into which the stream flows, such as a lake or ocean, or an artificial structure like a dam. At base level, erosion stops and sediment deposition begins.
Lowering a stream's base level will cause the stream to do what?
Lowering a stream's base level will cause the stream to do what?
The ultimate base level of a stream is sea level. A base level is the lowest point to which a stream can erode its channel.
The base level of a river is the lowest place where it can flow, generally it's mouth. Therefore if a river or stream flows into another river, then the first river's base level is the point where it joins the other river.
base level-The lowest level to which a stream can flow. :)
If you lower a stream base level it will cause a down cut. In some cases this is a good thing.
The type of bedrock can significantly affect the rate at which a stream erodes downwards towards its base level. Soft, easily erodible bedrock like clay or sandstone will result in quicker erosion and a faster rate of reaching base level than harder bedrock like granite or basalt, which will erode more slowly. Additionally, the presence of fault lines or fractures in the bedrock can also influence the speed at which a stream reaches its base level.
increases the vertical distance between the source and destination increasing energy.
Streams can't erode their channels endlessly. there is a lower limit to how deep can a stream erode. Base level is the lowest point to which a stream can erode its channels.