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Rivers.

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Presentation on theme: "Rivers."— Presentation transcript:

1 Rivers

2 Why important? Flooding has tormented civilization for a long time.

3 But… we continue to occupy low-lying regions adjacent to rivers.

4 Must understand ENTIRE river system… not just the region occupied by water on most days.

5 Drainage Basins: Where the water comes from.

6 Drainage Patterns

7 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

8 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

9 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

10 Channel Patterns – Braided Rivers
Nizina river, Alaska

11 Channel Patterns – Meandering River (forms & processes)

12 Avulsion – “permanent” change in a river’s course
1952 1988 McMurdo Basin, Columbia River, B.C.

13 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

14 Competence Diagram

15 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

16 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)

17 Florida Rivers

18 Florida Rivers


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