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From a longitudinal view, it is the deepest part of the riverbed from the source of the mouth. It is line of steepest descent along the streambed and is almost alway the line of fastest flow in any river

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What is the Thalweg?

A thalweg is the lowest elevation in a valley or watercourse.


What is lowest point called?

Thalweg


What is the rivers lowest point called?

Thalweg


How slip off slope formed?

thalweg >>> depositon >> inner bend


Where does the maximum velocity of water occur along the curve of a stream?

The maximum velocity of water typically occurs at the center of the stream where the flow is deepest and least affected by friction from the streambed and banks. This is known as the thalweg or thalweg line.


Where is the rivers velocity the highest?

The velocity of a river is typically highest in the center of the channel, where the water has the least amount of friction with the riverbanks and bed. This is known as the thalweg.


What is thalweg doctrine?

this principle is used to form international water boundary between nations having dispute over an region, it is also binding upon LAW OF SEA.


What is the main channel in a river called?

The "Main Channel".


What is the lowest point called?

Thalweg


What are fast-moving river called?

A fast flowing stream is called a rapid. Rapids are where the water flows downhill very fast and over underwater obstacles.


What is meander migration?

the side to sidecurves in a riverthat occur whenthe land is relativelyflatAs the river erodes quicker at the thalweg (the path of the fastest flowing water) and slower on the opposite banks, where it is depositing on the slip-off-slope, the river moves. It covers a large area over time as it moves and 'smooths out' the land.


Which location in a stream does dynamic equilibrium occur?

Dynamic equilibrium occurs at the point where the erosion and deposition of sediment are balanced, typically found in the middle or thalweg of a straight channel of a stream. At this location, the stream is in a state of dynamic equilibrium where the overall shape and characteristics of the channel remain relatively stable over time.