cuts mainly side to side
A floodplain forms where a stream overflows its banks during periods of high water flow, depositing sediments and creating a flat, fertile area on either side of the stream channel. This area is important for natural flood control and supporting diverse ecosystems.
its cool
A slowly flowing stream with wide meanders in a wide floodplain is typically in the mature stage of development. At this stage, the stream has developed its floodplain and exhibits significant lateral erosion, leading to pronounced meanders. The gentle gradient allows for slower water flow, contributing to the formation of these features.
A 'floodplain'.
The floodplain.
The stages of stream development are youthful, mature, and old age. In the youthful stage, the stream has a steep gradient with a narrow, V-shaped channel. In the mature stage, the stream has a meandering channel and a wider floodplain. In old age, the stream has a very flat gradient, a wide meandering channel, and a broad floodplain.
When a stream floods, it deposits much of the sediment that it carries onto its floodplain
floodplain
Meanders are created in the stream bed when a shallow graded stream cuts from side to side in its erosion process.It will create cliffs on the outside of the bends, and smooth banks on the inside of the stream. These features will migrate upstream.
A floodplain, or flood plain, is flat or nearly flat land adjacent to a stream or river that experiences occasional or periodic flooding.
Stream deposition occurs when a flowing stream loses energy, causing it to slow down and deposit sediment that it was previously carrying. This commonly occurs when the stream enters a flatter area, like a floodplain or a lake. As the stream's velocity decreases, it can no longer transport sediment, leading to deposition.
It cuts a wider, shallow channel .