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Streams (Rivers). Runoff: H 2 0 that does not sink into ground Most ends up in streams.

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Presentation on theme: "Streams (Rivers). Runoff: H 2 0 that does not sink into ground Most ends up in streams."— Presentation transcript:

1 Streams (Rivers)

2 Runoff: H 2 0 that does not sink into ground Most ends up in streams

3 How much, depends on terrain + amount of precip. Assume same precipitation for both. Which place would have More runoff?

4 Assume same precipitation for both. Which place would have More runoff?

5 Assume same precipitation for both. Which place would have More runoff?

6 People can increase runoff by: Removing vegetation (road building, bad farming, clear cutting)

7 Clear cut forest in Canada

8 Building large parking lots/buildings

9 Silt fence Water retention pond

10 Extra runoff can lead to: Loss of top soil Aquifers not being replenished (wells going dry) Flooding downstream

11 Load: Sediment carried by water Faster moving water carries more load

12 3 main types of load: 1.Dissolved: minerals like NaCl 2.Suspended: silt, clay (makes water look muddy) 3.Bed: sand, gravel Bed Dissolved Suspended

13 Types of streams: 1.Meandering streams: on low slopes, fine sediment

14 Point bar: sediment deposited in slow water

15 Cut bank: where sediment is carried away in fast water Draw and label fastslow fast slow fast

16 Oxbow lake: remnant of stream

17 2. Braided streams: bars and islands in middle

18 3. Mountain stream: steep slope, no floodplain, straighter

19 Drainage basin: area drained by a stream

20 Divide: separates basins Ex.: Rocky Mnts. called Continental Divide

21

22 North Carolina river basins

23 Tributary: smaller stream that empties into a larger one

24 Canyon formation: River cuts down as land is uplifted

25 Uplift of the Colorado Plateaus forced rivers to cut down faster

26 Stream Deposition: erosion load deposition produces

27 Delta: Sediment deposition when stream reaches its base level

28 Alluvial fan: deposition when a stream flattens out

29 Stream discharge: Volume of water flowing in m 3 /s (or cfm)

30 Floodplain: Land next to stream that floods periodically

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33 Dealing with floods has its problems.

34 1. Levees: ridges (natural or artificial ) that contain a stream

35

36 2. Channelizing can: Create flooding downstream Increase erosion Warm water by removing trees

37 Trap river organisms Trap sediment Expensive Flood land upstream 3. Dams:


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