When water is added to a stream table, a stream does not form immediately. The path of the stream is determined by factors like channel geometry and land gradient. Stream channels can vary in characteristics based on factors like erosion cycles and stream age.
When water is added to a stream table, a stream does not form immediately. Initially, the water may spread out and slowly move, showing characteristics of slow lateral flow.
The path of the stream is determined by various factors including the channel geometry and gradient of the land. As water flows around curves, the outside of the curve erodes while sediment is deposited on the inside, leading to the formation of a meandering stream over time.
Stream channels can vary in their characteristics, from straight to curved, deep and slow, or rapid and choked with sediments. These differences are influenced by factors such as the cycle of erosion and the stream's age.
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