River meandering is caused by the lateral movement of the river channel, which is driven by the force of the water flowing through the channel. As water flows around bends in the river, it erodes the outer bank and deposits sediment on the inner bank, causing the river to gradually change its course.

Point bars, riffles, and pools are all characteristic features of a meandering river. Point bars are sediment deposits that form on the inside of bends in the river, while riffles are shallow areas with fast-flowing water that occur at the heads of pools. Pools are deep areas of slow-moving water that occur at the tails of riffles.

Braiding is the process by which a river splits into multiple channels that rejoin downstream. This can occur when the river's sediment load is high, the riverbed is steep, or the river's flow is variable.

Mid-channel bars are characteristic features of braided rivers. These are sediment deposits that form in the middle of the river channel, often due to the deposition of sediment from upstream tributaries.

The primary factor that determines whether a river will meander or braid is a combination of the river's gradient, sediment load, and flow regime. Rivers with a low gradient, high sediment load, and variable flow regime are more likely to braid, while rivers with a high gradient, low sediment load, and steady flow regime are more likely to meander.

River meandering can have several negative impacts, including increased flooding, erosion of riverbanks, and loss of habitat for aquatic species. Meandering rivers are more prone to flooding because the sinuous course of the river can slow down the flow of water and cause it to back up. Erosion of riverbanks can also occur due to the lateral movement of the river channel, which can undermine and collapse the banks. Additionally, meandering rivers can create isolated pools and backwaters that can become stagnant and lose their value as habitat for aquatic species.

River meandering can have several positive impacts, including the creation of diverse habitats for aquatic species, improved water quality, and flood control. Meandering rivers create a variety of habitats, including pools, riffles, and point bars, which support a diverse array of aquatic species. The sinuous course of a meandering river also slows down the flow of water, which allows sediment and pollutants to settle out, improving water quality. Additionally, meandering rivers can help to control flooding by storing floodwaters in their floodplain.

Neck cutoff is the process by which a river's meanders become increasingly sinuous. This occurs when the river erodes the neck of a meander, causing the meander to be cut off from the main channel. The cutoff meander then becomes an oxbow lake.

Oxbow lakes are typically horseshoe-shaped, which is a characteristic feature of these landforms. This shape is created when a river's meander is cut off from the main channel, leaving behind a crescent-shaped body of water.

Incision is the process by which a braided river channel becomes narrower and deeper. This occurs when the river erodes its bed and banks, causing the channel to become entrenched. Incision can be caused by a variety of factors, including changes in the river's sediment load, flow regime, or gradient.

Incised river channels typically have steep banks, which is a characteristic feature of these landforms. This is because the river has eroded its bed and banks, causing the channel to become entrenched. The steep banks of an incised river channel can be unstable and prone to collapse.

Channel avulsion is the process by which a river changes its course suddenly and dramatically. This can occur when the river erodes its banks and creates a new channel, or when the river overflows its banks and floods a new area. Channel avulsion can be caused by a variety of factors, including changes in the river's sediment load, flow regime, or gradient.

Channel avulsion deposits typically contain levees, which are natural embankments that form along the banks of a river. Levees are created when the river overflows its banks and deposits sediment on the floodplain. Over time, these sediment deposits can build up and form levees that can help to protect the floodplain from flooding.

Aggradation is the process by which sediment is deposited on the floodplain during a flood. This occurs when the river overflows its banks and deposits sediment on the land. Aggradation can lead to the formation of floodplains, which are areas of land that are regularly flooded by a river.

Floodplains typically contain backswamps, which are areas of wetland that are formed when a river overflows its banks and floods the surrounding land. Backswamps are important habitats for a variety of aquatic and terrestrial species.