A. No meanders
B. Low stream gradient
C. No tributaries
D. Near headwaters
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Mar 6
1. Meandering flow pattern: Old rivers tend to have a meandering flow pattern with numerous bends and curves in their course.
2. Wide floodplains: Old rivers often have wide floodplains that have been formed over time by the river's meandering and shifting course.
3. Slow flow rate: Old rivers typically have a slower flow rate compared to younger, more energetic rivers.
4. Well-developed riverbanks: Old rivers often have well-developed riverbanks that have been shaped by erosion and deposition over time.
5. Mature vegetation: Old rivers tend to have mature vegetation along their banks and floodplains, as the ecosystem has had time to establish and develop.
6. Sediment deposition: Old rivers may have significant sediment deposition along their course, resulting in the formation of sandbars, islands, and other features.