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(,rivers, brooks, creeks, etc.)
Streams (,rivers, brooks, creeks, etc.)
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Processes Erosion Deposition
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Loads Bed load Suspended load Dissolved load gravel
rounder with greater working Suspended load silt Dissolved load salt, lime
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Load Carrying Capacity
Higher velocity flow allow stream to carry: larger particles more total load per volume
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What Happens When Deposition when flow slows
New erosion when flow speeds up
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Sorting Velocity changes gradually Slowing: deposit heaviest load
Speeding: remove lightest substrate Result: particles of same size found together (sorted)
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Common Profile Steep and fast in headwaters Slower near base
Cannot excavate below base level
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Drainage Patterns Determined by substrate characteristics Trellis
Dendritic Radial
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Stream Features
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Headlands V-shaped valleys Erosion dominates
Alluvial fan at foot of mountain
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Bottomlands Flat valleys Deposition dominates BUT—flow is variable
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Bottomland Features Floodplains Meanders Oxbows Levees Yazoo streams
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Meanders Erosion on outside Deposition on inside cutoffs Oxbows
cut bank Deposition on inside point bar cutoffs Oxbows
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Meandering River
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Meander Evolution
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Meander Evolution
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Meander Evolution
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Meander Evolution
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Meander Evolution
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Meander Evolution
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Meander Evolution
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Meander cutoff
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Oxbow lake
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Floods Normal Bank-full discharge ~ 2 years
Deposit on levees, flood plains
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Meandering river flooding
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Base Level Delta: deposits choke with sediment
many distributary channels lobes shift old sediments subside
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