Essentials of Fire Fighting, 5 th Edition Chapter 14 — Fire Streams Firefighter I.
Chapter 14: Streams and Floods Visit the Online Learning Centre at Chapter 14: Streams.
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Transcript of Chapter 14: Streams and Floods Visit the Online Learning Centre at Chapter 14: Streams.
Chapter 14: Streams and Floods
Visit the Online Learning Centre at www.mcgrawhill.ca/college/plummer
Chapter 14: Streams and Floods
What is the Hydrologic Cycle?What is the Hydrologic Cycle?What is a Stream?What is a Stream?
How do Drainage Patterns Reflect Geological Conditions?How do Drainage Patterns Reflect Geological Conditions?What Factors Affect Stream Erosion and Deposition?What Factors Affect Stream Erosion and Deposition?
How Does a Stream Erode?How Does a Stream Erode?How do Streams Transport Sediment?How do Streams Transport Sediment?Where do Streams Deposit Sediment?Where do Streams Deposit Sediment?
Can We Predict When Floods Will Occur?Can We Predict When Floods Will Occur?How Do Stream Valleys Change With Time?How Do Stream Valleys Change With Time?
Chapter 14: Streams and Floods
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The Hydrologic Cycle
Figure 14.1
Chapter 14: Streams and Floods
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Longitudinal and Cross-Sectionsof a Typical Stream
Figure 14.2
Chapter 14: Streams and Floods
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Drainage Basins of North America
Figure 14.4
Chapter 14: Streams and Floods
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Drainage Patterns Reveal SomethingAbout Rocks Underneath
Figure 14.5
Chapter 14: Streams and Floods
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Regions of MaximumVelocity in a Stream
Figure 14.6
Chapter 14: Streams and Floods
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Stream Velocities at Which Erosion and Deposition of Sediment Occur
Figure 14.7
Chapter 14: Streams and Floods
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Channel Shape and RoughnessInfluence Stream Velocity
Figure 14.8
Chapter 14: Streams and Floods
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Channel Width Variations Caused by Rock Type and Obstructions
Figure 14.9
Chapter 14: Streams and Floods
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Hydraulic Action Can Loosen, Roll, and Lift Grains from the Stream Bed
Figure 14.11
Chapter 14: Streams and Floods
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Sand and Gravel Moving on or near Stream Bed by Traction & Saltation
Figure 14.14
Chapter 14: Streams and Floods
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Flood Washes Away Bars in a Stream, Depositing New Bars
Figure 14.16
Chapter 14: Streams and Floods
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Types of Placer Deposits
Figure 14.17
Chapter 14: Streams and Floods
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Location Map of the Grand Canyon Controlled-Flood Experiment
Box 14.1, Figure 1
Chapter 14: Streams and Floods
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Graph of Annual Peak Discharges before (black) and after (blue) Glen Canyon Dam & 1996
Controlled High-Flow Release
Box 14.1, Figure 2
Chapter 14: Streams and Floods
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Cross-Section of the Channel Downstream of the Confluence with the
Little Colorado River
Box 14.1, Figure 3
Chapter 14: Streams and Floods
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(A) Midchannel Bar(B) Braided Stream
Figure 14.18
Chapter 14: Streams and Floods
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(A) Development of River Meanders and Point Bars; (B) Point Bar Deposit
Figure 14.22
Chapter 14: Streams and Floods
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Creation of an Oxbow Lake by a Meander-Neck Cutoff
Figure 14.23
Chapter 14: Streams and Floods
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Flood Plains
Figure 14.26
Chapter 14: Streams and Floods
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Natural Levee Deposition During a Flood
Figure 14.27
Chapter 14: Streams and Floods
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Internal Construction of a Small Delta
Figure 14.29
Chapter 14: Streams and Floods
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(A) Wave-Dominated Delta(B) Tidal-Dominated Delta
Figure 14.30
Chapter 14: Streams and Floods
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Alluvial Fan at theMouth of a Narrow Canyon
Figure 14.31
Chapter 14: Streams and Floods
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Annual Peak Discharge for the Red River, MB, from 1892-1999
Box 14.3, Figure 1
Chapter 14: Streams and Floods
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Flood-Frequency Curvesfor the Red River
Box 14.3, Figure 3
Chapter 14: Streams and Floods
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Urbanization can Increasethe Chance of Floods
Figure 14.33
Chapter 14: Streams and Floods
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1976 Flash Flood on Big Thompson River and 1997 Flash Flood in Fort Collins
Figure 14.34
Chapter 14: Streams and Floods
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Examples of Flood-Control Structures
Figure 14.36
Chapter 14: Streams and Floods
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Downcutting, Mass Wasting, and Sheet Erosion Shape Canyons and Valleys
Figure 14.37 (A) and (C)
Chapter 14: Streams and Floods
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Base Level is the Lowest Level of Downcutting
Figure 14.38
Chapter 14: Streams and Floods
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Ungraded and Graded Streams
Figure 14.39
Chapter 14: Streams and Floods
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Lateral Erosion Widens Valleys by Undercutting and Eroding Walls
Figure 14.40
Chapter 14: Streams and Floods
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Terraces Formed by a StreamCutting Downward into itsOwn Flood-Plain Deposits
Figure 14.43
Chapter 14: Streams and Floods
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Incised Meanders can Form by Uplift
Figure 14.45
Chapter 14: Streams and Floods
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Development of a Superposed Stream
Figure 14.46
Chapter 14: Streams and Floods
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Answers to SelectedTesting Your Knowledge
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Chapter 14: Streams and Floods
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Additional Resources
Student ResourcesStudent ResourcesStudent Online Learning CentreThe robust Student Edition of the Online Learning Centre at www.mcgrawhill.ca/college/plummer features quizzes for study and review, interactive exercises and animation, as well as additional boxed readings, searchable glossary, “Virtual Vista” environments, suggestions for further reading, and much more!
Laboratory ManualThe Lab Manual to accompany Physical Geology and the Environment has been created as a resource for laboratory sessions in physical geology, mirroring the "Inquiry-Based Approach" of the text. Structured on exercises and corresponding background concepts, the lab manual contains student-friendly worksheets, and has been perforated for easy lab use.
Instructor ResourcesInstructor ResourcesInstructor Online Learning CentreThe OLC at www.mcgrawhill.ca/college/plummer includes a password-protected Web site for Instructors. The site offers downloadable supplements and access to PageOut, the McGraw-Hill Ryerson Web site development centre.
Instructor’s Manual – The IM contains a chapter overview, list of changes per chapter, chapter learning objectives, further information on boxed features, short and long discussion/essay questions, and details on additional readings and resources outside the textbook.
Test Bank – Contains a bank of 40-60 multiple-choice and true/false questions per chapter.
Microsoft PowerPoint Presentation – This presentation system offers visual presentations that may be edited and manipulated to fit a particular course format. They also contain selected solutions to the problem material.
TransparenciesA set of more than 200 transparencies tied to the text content are available for instructors.