The water usually flows fastest on the outside of the bend (meander) and flows the slowest on th einside of the bend.
The outer curve.
The side of a meander that it flows faster is in the clean water than in the dirty water
Erosion primarily occurs on the outside curve (cutbank) of a meander, where the water flow is faster and more forceful. Deposition occurs on the inside curve (point bar) of the meander, where the water flow is slower, allowing sediment to be deposited.
the flow of the river.
No
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)).
A river's flow tends to slow down on reaching a flat valley floor. It is here that the river may meander, creating bends and ox-bow lakes.
A river's flow tends to slow down on reaching a flat valley floor. It is here that the river may meander, creating bends and ox-bow lakes.
A meander is a bend in the coarse of the water flow in a river. There is not a river recorded with the most meanders, although rivers with the most meanders are located in Africa.
serpentear -> to meander Serpenteo = I meander Serpenteando = meandering Serpenteas = You meander Serpentea = He/ She/ You (formal) meander(s) Serpenteamos = We meander Serpenteáis = You (plural) meander Serpentean= They/ you (plural, formal) meander
A meander is described to as a river or stream with eroded banks such that it no longer flows in a relatively straight path, but instead is a winding path.
Because it has further to travel