Meandering River. Meanders are the result of both erosional and depositional processes. Alluvial fan drainage divide oxbow lake basin drainage pattern sinuosity braided streams entrenched meander stream discharge cutbanks hydrograph stream.
Meanders named from the menderes historically known as the maeander river in turkey are most often formed in alluvial materials stream deposited sediments and thus freely adjust their shapes and shift downstream according to the slope of the alluvial valley. The main characteristic of the trough stage of a river is to form meanders. There is a differentiation in flow speeds within a meandering river channel that produces areas of erosion and deposition.
Identify the physical features common to a meandering river system module to learn how to maneuver through and how to answer the lab questions in the google earth component.
This causes individual meanders to grow larger and larger over time. Meanders are the result of both erosional and depositional processes. Figure 14 1 shows a full meander length. These are called meandering rivers.
