Levees and regoliths.
the sand, gravel, boulders, or other debris transported by rolling or sliding along the bot-tom of a stream.
PIE not the pi in math but,PIE as in the thanksgiving pie you have after your turkey,stuffing, and mashed potatoes. PIE!!
Alluvial Fan
On the outside. This is because when the water is flowing around a meander, the water practically goes around, where erosion occurs. If you know science, wherever in a stream where erosion occurs, thats where the velocity is greatest.
conglomerate
The river's velocity is much slower on the inside bend of a meander, so any material being transported in the river is deposited.
Deposition in a meander of a stream occurs most prominently on the inside bend of the meander. Here, the flow of water is slower, allowing sediment to settle and accumulate. As the water curves, the outer bank experiences erosion due to faster flowing water, while the inner bank builds up with deposited materials. This dynamic leads to the formation of point bars on the inside bends.
i think you mean stream meander. the process is deposition
Point Bar
Coarse sediment, such as gravel and larger particles, is typically deposited first in a stream channel due to its heavier weight and inability to remain suspended in the flowing water for extended periods of time. Finer sediment, like sand and silt, may be carried further downstream before being deposited.
A deposit of sediment that forms on the inside of a stream meander is known as a point bar. As water flows around the meander, the velocity decreases on the inside bend, causing sediment to settle and accumulate. Over time, this buildup can create a small, sandy or gravelly landform that may support vegetation and alter the stream's flow dynamics. Point bars are important for habitat diversity and can indicate changes in the river's sediment transport processes.
The part of a stream that will experience a buildup of sand and gravel is typically the inside bend of a meander, known as a point bar. As water flows around the bend, it slows down, leading to decreased energy and allowing sediment to settle and accumulate. This contrasts with the outside bend, where the current is faster and erosion occurs. Additionally, areas where the stream widens or slows down, such as floodplains, can also experience sediment deposition.
Larger particles are deposited first as a stream loses velocity. Gravel would be deposited first, since it is the largest (out of Clay, Silt, Sand, and Gravel)
An esker is a long, winding ridge of sand and gravel deposited by a melting glacier. It is typically formed in tunnels within or beneath the ice and can stretch for many kilometers. Eskers are a common feature in glaciated regions.
Deposition occurs on the point bar in a meandering stream. The point bar is located in the inside of the bend of a meander where the current is the slowest. The slower current allows for deposition.
In a stream channel, the coarsest materials, such as gravel and larger sediments, are typically deposited first. This occurs because these heavier particles require more energy to be transported and settle out of the water when the stream's velocity decreases. As the flow slows down further, finer materials like sand, silt, and clay are deposited afterward. The sorting of sediments in this manner reflects the energy dynamics of the stream.
Sediments like sand and gravel are typically deposited first in a stream channel due to their heavier weight and larger size compared to finer particles like silt and clay. These sediments settle out when the stream's velocity decreases, usually in areas with reduced flow or obstacles that disrupt the current.