numbers htat rrrr 1846573928429835r394876w89085=49t94869048790860458658609788908790798908795685905748578957689035809048
The wearing down of soil and bedrock of a river or stream creates a channel, which is a trough or groove formed by the flow of water. This channel path is where the river or stream flows and carries sediment downstream. Over time, erosion can widen and deepen the channel, shaping the landscape.
A river, or stream.
A river channel is formed by rock and soil of a stream being transported down, during this process the channels become wider and deeper.
A channel through which water is continually flowing downhill is a stream. A large channel in soil that carries runoff after a rainstorm is a gully.
A stream's base level is the lowest point to which it can erode its channel, typically the level of a lake, river, or ocean. When the base level drops, a stream can cut down more deeply into its channel, increasing its gradient and potentially leading to features like waterfalls or canyons. Conversely, if the base level rises, the stream may have less energy to erode and can begin to deposit sediment, leading to a more meandering channel. Thus, the base level plays a crucial role in determining the stream's erosional power and channel morphology.
A stream.
a little bed of water flows and the joins a bigger bed of water, where it joins a stream and then another stream to a bigger stream, then a river which joins a bigger river then goes down to a waterfall where it joins a lake.
A channel where water is continuously flowing down a hill would be described as a stream, or possibly a rivulet, depending on its size.
when the river is carrying vast amounts of erdoded material as bedload. as water levels fall and the energy decreases the river drops its coursest material. the rapid deposition of its coursest material begins to block the main channel causing the river to divide into smaller channels that seek to find the way through the obsructing channel
The Mississippi River has three stages: First, it is a youthful river, further down the stream it comes into its mature stage, and even further down the river, at the end, it comes into its old age stage. All rivers have three stages, it just depends what part of the river you are looking at.
Because there strong enough
meander