Final answer:
Meandering streams have a sinuous pattern in the channel, with erosion and deposition creating specific landforms such as cut banks, point bars, and oxbow lakes.
Step-by-step explanation:
The flow characteristics of a meandering stream involve a sinuous or winding pattern in the channel. This is caused by the erosion and deposition of sediment along the banks of the stream. As the stream flows, it erodes the outer banks, creating a cut bank, and deposits sediment on the inner banks, creating a point bar.
The erosional features of a meandering stream include cut banks, which are steep slopes on the outer curve of a meander, and meander scars, which are abandoned segments of the channel. The depositional features include point bars, which are depositional landforms on the inner curve of a meander, and oxbow lakes, which are cut-off meanders that become isolated from the main channel.
The typical landforms created by meandering streams include flood plains, which are flat areas adjacent to the channel that are subject to periodic flooding, and meander belts, which are a series of alternating meanders along the course of the stream.