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Study Guide Chapter 17 1.Know and use the simple equation for discharge. Why is this equation important? 2.What is the gradient of a stream? 3.Describe.

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Presentation on theme: "Study Guide Chapter 17 1.Know and use the simple equation for discharge. Why is this equation important? 2.What is the gradient of a stream? 3.Describe."— Presentation transcript:

1 Study Guide Chapter 17 1.Know and use the simple equation for discharge. Why is this equation important? 2.What is the gradient of a stream? 3.Describe the means of stream transportation. Describe the type of material transported by each load type. 4.Describe the features of upper, middle, and lower course of a river. 5.Describe the 6 patterns that streams form and how these patterns are formed. 6.Be able to distinguish stream order on a topographic map. What are the differences between a first order stream and second order stream. 7. What is drainage density 8. Interpret a hydrograph. 9. What is a yazoo stream, oxbow lake, delta, and levee? 10. Describe a drainage basin/watershed, interfluve, and divide.

2 Fluvial Processes and Landforms Stream is a general term for water in a channel. We call a large stream a river. Fluvial processes are any work done by a stream. Gradient of stream is the vertical drop.

3 A Drainage Basin/Watershed- Land surface drained by a stream system Line of demarcation Higher ground between valleys

4 Stream flow Discharge- The amount of water passing a particular point per unit time. Q= AXV where Q is discharge in ft 3 /sec CFS (cubic feet per second), A is the cross sectional area of the stream ft 2, and V is the velocity of the stream ft/sec A= width (ft. ) X depth of stream (ft.) Gauging stations (Fig. 17.6) maintained by Department of Public Works or USGS.

5 Stream Transportation Figure 17.15 Dissolved Load Finer particles Gravel or pebbles

6 Stream Transportation Upper course –More gradient and more energy –V shaped valleys formed from erosion (Fig. 17.20) Middle Course –Meandering of stream –Reduced gradient/decreased energy Lower Course –Vast floodplain. –Yazoo stream, oxbow lake, delta, Levee

7 Zones of a River Rain and snow Source Zone Water Sediment Lake GlacierRapids Waterfall Tributary Flood plain Oxbow lake Salt marsh Delta Ocean Deposited sediment Transition Zone/Middle Zone Flood-Plain Zone Fig. 7.17, p. 168 Upper Course Lower course

8 Upper Course

9 Floodplain Features/Lower course of River Figure 17.26 Parallel to main river levee

10 Nile River Delta Figure 14.25 Triangular arc shape

11 Fig. 17-7, p. 476

12 Fig. 17-5, p. 475 Stream ordering

13 Fig. 17-8, p. 477 Drainage Patterns


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