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the difference in velocity is mostly due to the great efficiency of the large downstream channel.
Speed and direction determine velocity
At what depth should a velocity sensor be placed to estimate a stream's average velocity if it is 12.5 meters deep?
Size of the sand grains and velocity of the stream
increase
Decrease in stream velocity
Deposition, whereby the sediment load being transported is dropped.
It cuts a wider, shallow channel .
sediments are transported by ocean rift, streams, river currents, wind (air). they are deposited according to size. The largest sediments are deposited first. The sediments settle into the sand and are carried by the stream. Near the mouth of the stream where the water moves slowly the small sediments settle out. The larger sediments get carried by the river into the sea then the samller sediments. The sea water dissolved minerals and soak the sediments and cement together. This eventually forms sediments.
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.
Generally the speed of the transported load slows down considerably with the change in the transport medium from stream to lake or sea. As the energy of the motion is reduced, gravity claims the sediments.
In a stream, heavy sediments settle quickly and finer sediments stay suspended in the water and get carried down stream farther, even as the stream shrinks in size.
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.
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.
An increase in gradient will generally increase stream velocity.
Little sediments are carried by the eroding stream