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Stream transport sediment in three ways, dissolved load, (ions in solution being carried downstream), suspended load, (suspended sediment that floats freely downstream) and bed load, (sediment that rolls or scoots along the bottom of the river).
In contemporary English, there is no single term that denotes authoritatively the direction in which a stream or river flows. 'Stream-flow' may be used; however, 'downstream' is practically applicable and commonly used, along with a number of other equivalent terms.
Sediment that is carried by a stream along the bottom of its channel.
The su polar low lies along the polar jet stream :)
Net osmotic pressure stays about the same and net hydrostatic pressure decreases.
stream turns into green water
called a bed load its sediment that moves along the bed of a stream by rolling bouncing or sliding
stream turns into green water
Electropositivity decreases along a period. The metallic character also decreases.
erosion
All streams meander to some extent. The most likely time is when flow is consistent and gradient is uniform. See Braided Stream. When a stream has eroded the steep valleys to genteler slopes, the stream flows more slowly.Now water in the stream erodes along the sides of the stream bed rather than along the stream bottom. === ===
no