It cuts a wider, shallow channel .
There are three factors that affect stream erosion. These are water velocity, shape, size and depth of channel, and stream capacity to transport eroded materials.
The Velocity
As water in the stream channel flows, it encounters friction; the friction slows the forward movement. The shape,size, and roughness affect the amount of friction. High friction slows the stream significantly.
the difference in velocity is mostly due to the great efficiency of the large downstream channel.
When the discharge of a stream increases, so does it's velocity. When it decreases, so does the velocity.
the competence and capacity of a steam depend on a streams velocity and discharge. Because the velocity and discharge of a given stream are not constant , the competence and capacity of a stream are not constant . competence and capacity vary along a stream and change throughout the year.
Stream discharge is a product of the velocity and the area of the stream (velocity x width x depth), and has units of volume per time (e.g. cubic feet per second, cubic meter per day, etc). Stream velocity is the vector describing the speed of the water and has units of length per time (feet per second, meter per second). Stream discharge is relatively constant as you move up and down a stream, while velocity will change predominately as you change depth. The velocity of water is lowest near the bed of the stream, and highest at the surface.
The velocity of the water in a stream increases when the stream gets narrower or shallower (or both).
Stream load is when solid matter is carried by a stream. Stream capacity depends on the velocity, the amount of water flow and the grade.
After a stream's discharge increases, it overflows its banks and a flood occurs.
An increase in gradient will generally increase stream velocity.
On the inner curve of a meander, where the velocity of the water is the slowest.