Meanders are sinuous, winding curves or loops in a river's course. They are typically found in the middle and lower courses of a river where the gradient is lower and the river has more lateral erosional and depositional processes.
Meanders form as a result of a combination of erosion, transportation, and deposition processes. As a river flows, it erodes the outer bank on the outside of a bend through a process called lateral erosion, and deposits sediment on the inner bank through a process called deposition. Over time, this causes the river to form a curved, meandering path.
Meanders are characterized by a few key features:
To understand meanders better, consider the following study guide:
Understanding meanders is essential for comprehending river dynamics and landform evolution. It also provides insights into the interactions between rivers and their surrounding environments.