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Rivers
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Why important? Flooding has tormented civilization for a long time.
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But… we continue to occupy low-lying regions adjacent to rivers.
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Must understand ENTIRE river system… not just the region occupied by water on most days.
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Drainage Basins: Where the water comes from.
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Drainage Patterns
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Basic Terminology: Flood plain -area adjacent to river channel Streams and Rivers Runoff-portion of moving across the surface Drainage basin -area drained by single stream Slope-gradient of a stream (drop/unit of length) Longitudinal profile -plot of elev. vs. length Cross-section- profile across a stream valley Plan view- two dimensions, map view Base level- lowest level that a stream can erode its bed Stream power = discharge X slope X unit weight of water
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Measuring and Calculating Discharge
Continuity Equation Discharge Q= V x A or V x W x D blackboard example of conservation of discharge Reach -river area under study
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Channel Patterns Channel Patterns Braided Meandering Point bars
Riffles and pools Oxbows Anastomosing Multiple channels Gulf Coast (Fl, La) Riverine environment--the river and adjacent floodplain
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Channel Patterns – Braided Rivers
Nizina river, Alaska
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Channel Patterns – Meandering River (forms & processes)
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Avulsion – “permanent” change in a river’s course
1952 1988 McMurdo Basin, Columbia River, B.C.
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Sediments in Rivers Streams and Rivers Transport of rock cycle
Erosion and sediments Total load Suspended load Bed load Dissolved load Competence-largest particle a stream can transport Capacity-total load a stream can carry
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Competence Diagram
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Velocity/Shear Stress, Erosion, and Deposits
Alluvial fan-change in slope Bajada -coalescing alluvial fans Delta -form at the mouth of some rivers Distributaries -streams that flow on deltas
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Effects of Land Use Change
Change in stream profiles Development Dam construction Modification of Continuity Equation Q = C x i x A (C = Coefficient of infiltration; i =intensity of rainfall; A-area)
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Florida Rivers
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Florida Rivers
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