erosion
flooding seems more accurate.
The river cliff is the outside of a meander in a river. This is due to erosion from fast flowing water. Deposition occurs on the inside and the inside bend is called the SLIP-OFF SLOPE
A meander is a bend in a river which will eventually erode to form an ox-bow lake which is a thing in a river! A meander is formed around a ox-bow lake. Your Welcome!! ;)
A meander is a bend or such like in a river
The river's velocity is much slower on the inside bend of a meander, so any material being transported in the river is deposited.
Erosion occurs in meanders and fast flowing parts of the river. Deposition occurs when the flow is too slow to carry the particles so drops the dirt and soil it is carrying. Deposition also occurs on the inside of a meander, which is why the meander stays the same width, but moves about.
A crescent-shaped lake formed by a river meander is called an oxbow lake. It occurs when a meandering river cuts off a meander bend, forming a U-shaped body of water separated from the main river channel. Oxbow lakes are often found in flat landscapes and are a natural part of a river's evolution.
As a river deposits sediment on the inside of a meander and erodes the outside of the meander, the meander migrates toward the outside edge
A bend in a river.
An isolated meander, often referred to as an oxbow lake, is a crescent-shaped lake that forms when a river meander is cut off from the main channel due to sediment deposition or erosion. This typically occurs when a river's course shifts, leaving behind a stagnant body of water that resembles a meander. Over time, the isolated meander can become ecologically distinct, hosting unique plant and animal communities. These formations are significant for understanding river dynamics and habitat diversity.
River bends are called 'esses' or 'meanders'
Meanders are bends in a river or watercourse. Meanders are more likely to be found in slower moving rivers. They often form ox-bows.
In a river meander bend, the fastest flow typically occurs on the outer bank of the bend. This is due to the centrifugal force acting on the water as it navigates the curve, causing increased velocity. In contrast, the inner bank experiences slower flow and sediment deposition, which can lead to the formation of point bars. This dynamic creates a characteristic pattern of erosion and deposition along meandering rivers.