while taking turn on the road,a car moves in a circular path to keep the car moving along the circular path, centripetal force is required. in the absence of this force, the car will skid off the road to the outer size of the road and may possibly turn turtle due to inertia .the force of friction between the tires and roads provides the necessary centripetal force and keeps the car moving on the curved path.
When a brook encounters curves on its banks, it tends to meander or snake along the bends. Erosion may occur on the outer bank of a curve, depositing sediment on the inner bank. This can lead to the creation of point bars on the inner bank and cut banks on the outer bank, influencing the shape and direction of the stream as it moves around the curves.
Over time, erosion and sediment deposition can cause one bank of a river to become slightly higher than the other. Factors such as the direction of the river's flow, the type of rocks and sediments in the area, and human activities can also contribute to this elevation difference.
Oxbows are formed by the meandering of rivers. As a river flows, it erodes the outer bank of a bend and deposits sediment on the inner bank, causing the bend to become more pronounced over time. Eventually, the meander may become so pronounced that the river cuts off the bend, forming an oxbow lake.
The side of a meander that it flows faster is in the clean water than in the dirty water
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The sediments removed from the outer bank are carried forward by the flow of the water to the inner bank and deposited. •Deposition occurs because the friction between the inner bank and the water is greater than at the outer bank, thus reducing its velocity. •With successive deposition, the water at the inner bank gets shallower, resulting in a slip-off slope.
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.
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.
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.
When a brook encounters curves on its banks, it tends to meander or snake along the bends. Erosion may occur on the outer bank of a curve, depositing sediment on the inner bank. This can lead to the creation of point bars on the inner bank and cut banks on the outer bank, influencing the shape and direction of the stream as it moves around the curves.
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.
The fastest part of a meandering river is typically on the outside of a bend where the water accelerates due to the increased centrifugal force. This faster flow erodes the outer bank of the bend and deposits sediment on the inner bank.
Over time, erosion and sediment deposition can cause one bank of a river to become slightly higher than the other. Factors such as the direction of the river's flow, the type of rocks and sediments in the area, and human activities can also contribute to this elevation difference.
As the river winds from side to side, it tends to erode the outer bank and deposit sediment on the inner bank of the bend. Over time, the meander becomes more and more curved.
Sediment would likely be eroded from the outer bank of a meander bend to help form an oxbow lake. As the river flows around a bend, the water on the outer bank moves faster, leading to erosion of the bank and deposition of sediment on the inner bank, eventually creating the oxbow shape.
The area of Outer Trial Bank is 42,650.0 square meters.
A meander is primarily created by erosion along the outer bank of a river bend and deposition along the inner bank. The flow of the water in a river directs erosional forces towards the outer bank, causing it to erode and form a bend in the course of the river.