it is called deposition
The inside bend of a river is called a "meander." Meanders occur as a result of erosion and sediment deposition along the riverbank, creating a curving or winding pattern in the waterway.
The process that occurs inside the chloroplasts is called photosynthesis. This process involves converting light energy into chemical energy by utilizing water and carbon dioxide to produce glucose and oxygen.
The inside of a meander bend is where the water flows more slowly, causing deposition of sediment, resulting in a point bar. The outside of a meander bend is where the water flows faster, causing erosion of the riverbank, forming a cut bank.
deposition occurs at the part of a river where there is no longer enough energy for the water to carry the sediments and they are deposited. Deposition is when an agent or erosion (in this case river water) loses energy and can no longer carry sediments, so it deposits them.
A river's current slow down and tend to meander across a flat valley floor. The river's current is faster on the outside of the bend, and slower on the inside.
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
i think you mean stream meander. the process is deposition
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.
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.
The inside bend of a river is called a "meander." Meanders occur as a result of erosion and sediment deposition along the riverbank, creating a curving or winding pattern in the waterway.
A gently inclining area formed on the inside of a meander is known as a point bar. It is created by the deposition of sediment as water slows down when it flows around the bend of the meander. This sediment accumulation gradually builds up, forming a gentle slope that contrasts with the steeper bank on the outside of the meander, where erosion typically occurs. Point bars are important for creating diverse habitats in river ecosystems.
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
on the inside of the bend
On the outer bank (at the tip of the meander)
The process that occurs inside the chloroplasts is called photosynthesis. This process involves converting light energy into chemical energy by utilizing water and carbon dioxide to produce glucose and oxygen.
Water deposits more on the inside of a meander due to the reduced flow velocity in that area. As a river bends, the outer bank experiences faster water flow, which can erode the bank and carry sediment downstream. In contrast, the inner bank has slower-moving water, allowing sediment to settle and accumulate. This process creates features like point bars on the inside of the meander.
deposition