Rivers "carry" their sediment load only as long as the velocity of the water remains high enough to create sufficient turbulence to keep the particles "stirred up". Once a river loses its velocity and the stirring effect of the turbulence subsides the sediment load can no longer remain suspended in the water. At this point gravity takes over and the river begins to "drop" its sediments in a process named deposition.
Now a river going around a curve is like two tires at each end of an axle going around a curve. The tire on the outside of the curve has to move faster than the tire on the inside of the curve since it has a longer radius of travel. So too the water in the river moves faster at the outside of the curve than the water inside the curve. Between the two different water velocities the deposition is going to occur on the inside curve of the river where the water loses its velocity.
Conversely, the opposite of deposition which is erosion will take place at the outside of the curve in the river.
They erode sediments when it snakes back and forth across their valley. xxxJoanna
These are glaciers.
The base level
It erodes rocks on steep hills because the rain is slightly acidic so the acid (carbonic acid) and when the rain falls on those rocks it dissolves them slowing turning them into sediment! :) +++ Not quite. Carbonic acid only attacks calcium carbonate, magnesium carbonate and calcium sulphate (the essential minerals of limestone & chalk, dolomite and gypsum, respectively), although water will hydrolyse some other rock minerals very slowly. The dissolved minerals are carried away in solution, not as sediment; but the rocks' insoluble constituents do become sediment. An upland stream can erode rock rapidly thanks to its higher gradient hence speed, but against that the further uphill you find the stream, the smaller its volume.
abrasion or the wearing away of rock by a grinding action.
Streams can't erode their channels endlessly. there is a lower limit to how deep can a stream erode. Base level is the lowest point to which a stream can erode its channels.
Are you talking about meanders? when overtime laterally erode the banks (undermine) due to the hydrolic fore of the water. Then then turn to ox-bow lakes due to deposition along the curve and erosion coming into the curve. (bypasses the curve; cuts straight through)
The outer banks can erode, especially the outside edge of a curve in the river. The bottom can also be down cut.
probably erode it lol
It starts to erode the boulder.
Erode
They erode sediments when it snakes back and forth across their valley. xxxJoanna
Streams can't erode their channels endlessly. there is a lower limit to how deep can a stream erode. Base level is the lowest point to which a stream can erode its channels.
These are glaciers.
The factors that affect a river's ability to erode and carry sediment would be its size, how deep it is, and how fast it is going. If it is going downhill that can also affect it.
Stream erode their channels by abrasion, grinding, and by dissolving soluble material.
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