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Explore the intricate world of river systems, from drainage basins to stream flow dynamics, erosion, deposition, and unique features like alluvial fans and deltas. Learn about the factors shaping rivers and streams' behavior and the fascinating processes at play. Uncover the secrets of meandering streams, braided channels, floodplains, and more.
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River Systems • A river or stream: any body of water flowing downhill in a well defined channel • Drainage basin • Drainage divide
Divided into 3 subsystems • Collecting system • Transporting system • Dispersing system
Stream System Order -Tributaries decreases downstream -Tributary length increases downstream -Gradient decreases downstream -Channels are wider deeper downstream
Common Drainage Patterns
Stream Flow Dynamics • Factors affecting stream behavior • Discharge (Q) • Gradient • Average velocity (V) • Channel cross-sectional area (A) • Load • Base level
Stream Flow Dynamics • Discharge • The volume of water flowing past a given point in the river • Discharge will vary with time and weather conditions • Measured in cubic meters per second
Gradient • The slope of the stream channel • Change in elevation divided by distance (m/km) • Longitudinal profile is a concave upward • Steep at headwaters • Nearly flat at discharge area
Velocity varies within the channel • Highest velocity is in the center of the channel • Drag slows water along the bottom, banks, and top (water-air interface)
Load • Material carried along by the stream • Suspended load (fine particles) or • Bed load (coarse particles) • Dissolved load (ions in solution)
Stream Erosion • River systems erode the land surface by: • Removal of weathering products • Downcutting of stream channel • Headward erosion
Downcutting of Channels • Bottom of stream channel abraded by transported sand & gravel
Headward Erosion • Erosion rates are greatest where stream gradients are high
Stream Deposition • Floodplains • Deltas • Alluvial valleys and fans
Meandering Streams • Rivers flow in a sinuous pattern • Turbulent flow & velocity changes eroded one bank, deposit on the other • Erosion changes course of river
River at Flood Stage Floodplain Main Channel
Floodplains • Floods • Normal stage - water level below the bank • Bankfull stage - water level even with the bank • Flood stage - water level above the bank • Floodplains • Areas that will be submerged when a river is at flood stage
Braided Streams • Multiple channel system • Interlaced channels with islands • High sediment load • Common in arid & semi-arid regions • Seasonal high flows • Common in front of glaciers • Large sediment load, fluctuating water flow
Alluvial Valleys • Streams fill part of their valleys with sediment • Changes in hydrologic conditions initiate deposition • Subsequently cut through deposits • Create terraces
Deltas • Formed by sudden drop in velocity • Stream enters ocean or lake • Stream drops sediment load • Evolve by three mechanisms • Growth may be influenced by ocean waves
Delta Growth • Distributaries • Levee and in-stream deposit formation • Channel splits into two smaller channels • Splays • Crevasse allow water to leave main channel • Water spreads out forming a splay deposit • Avulsion • Shift in main course to follow steeper slope
Alluvial Fans • Accumulation of sediment in a dry basin • Deposition due to rapid velocity drop • Usually arid climate • High sediment load - braided streams • Form fan-shaped deposit