The river flows the fastest in the middle of the river.
The fastest part of a meandering river is typically on the outside of a bend where the water accelerates due to the increased centrifugal force. This faster flow erodes the outer bank of the bend and deposits sediment on the inner bank.
Usually it is the upper reaches (often termed as mountain streams) that flow the fastest. In the lower, flatter valleys, rivers tend to slow down (except in spate, when the river is in flood)).
The velocity of a stream is usually fastest in the middle of the channel, away from the banks where friction against the sides slows down the water flow. This is due to lower friction and more space for the water to flow without obstruction.
through middle asia
right in the center of the steam because of the less friction
Laminar flow.
The Huang hu river in China, Ganges in india and Satluj in Himalayas are world's fastest flowing rivers with a speed of water flow crossing over 145Km/hour also.
dont know
Meandering characterized a river's course when its flow begins to slow. Meanders form when slight irregularities in the flow cause the moving water to be directed towards a bank. This bank then erodes and at this point the river gets wider and the flow slows causing sediment to be deposited against the opposite bank. Eventually the process causes a large bend in the river and the river develops meanders.
The main erosion at a bend in a river or meandering channel is known as lateral erosion. This occurs on the outside of the curve where the water flow is fastest, leading to the wearing away of the outer bank through the process of hydraulic action and abrasion.
in the middle course.if a river hits something and if it is slow then it is forsed to flow in curves known as meanders.
Over time, erosion and sediment deposition can cause one bank of a river to become slightly higher than the other. Factors such as the direction of the river's flow, the type of rocks and sediments in the area, and human activities can also contribute to this elevation difference.