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)
A bend or curve in a stream's channel caused by erosion is known as a meander. Meanders occur as the flowing water erodes the outer bank of a curve and deposits sediment on the inner bank, leading to a pronounced bend in the channel over time. Meanders are common in rivers and streams with gentle slopes and can contribute to the formation of oxbow lakes.
A curve in a stream channel is called a meander. Meanders are caused by the flow of water eroding the outside of a bend and depositing sediment on the inside, leading to a winding pattern in the channel. Meanders are a natural feature of rivers and streams and play a vital role in shaping the landscape.
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.
In a meander, erosion occurs on the outer bank of the curve due to higher velocity of water, which undercuts the bank. Deposition happens on the inner bank where the lower velocity of water leads to sediment accumulation. Over time, these processes cause the meander to elongate and create a more pronounced loop in the river.
Meander formation Water flows faster on the outer curve of the bend of a river and slower on the inner curve so the outer bank gets eroded, but silt is deposited at the inner bank. Over time as the outer bank wears and the inner one grows, a meander forms. As the process continues, the meander becomes more loopy. If you doing this for work/school I suggest you use diagrams/pictures to show each stage.
stream channel
A bend or curve in a stream's channel caused by erosion is known as a meander. Meanders occur as the flowing water erodes the outer bank of a curve and deposits sediment on the inner bank, leading to a pronounced bend in the channel over time. Meanders are common in rivers and streams with gentle slopes and can contribute to the formation of oxbow lakes.
A curve in a stream channel is called a meander. Meanders are caused by the flow of water eroding the outside of a bend and depositing sediment on the inside, leading to a winding pattern in the channel. Meanders are a natural feature of rivers and streams and play a vital role in shaping the landscape.
A mature stream causes more erosion than a young stream, due to the pure fact that theres more curve in a mature stream causing the sediments to shift more frequently.
Since the outside curve has a higher velocity, it has more erosion meaning the inside curve has a slower velocity more deposition causing it to be shallower. The outside curve is deep.
The outside curve of a stream is typically deeper than the inside curve. This occurs due to the erosion of the bank on the outer side, where the water flows faster and has more energy to remove sediment. Conversely, the inside curve experiences slower water flow, leading to sediment deposition and a shallower depth.
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.
Meander
The curve formed when water erodes one side of a stream is called a "meander." As the water flows, it exerts more force on the outer bank, leading to increased erosion there, while sediment is deposited on the inner bank, creating a bend in the stream. This process can lead to the formation of pronounced curves over time, contributing to the characteristic winding shape of meandering rivers.
The river is often deeper on one side of the channel due to the process of erosion and sediment deposition. As water flows, it moves faster on the outside curve of a bend, eroding the bank and creating a deeper channel. Conversely, the inside curve has slower water flow, leading to sediment deposition and a shallower area. This dynamic is part of the natural meandering process of rivers.
the middle curve
A change in price level would cause movement along the demand curve, but would not cause the curve itself to shift.