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Drifting Classroom

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Referring to your fieldwork results, what is the direction of river erosion in your field site? How does it affect the river channel? Explain ... Saltation. ... – PowerPoint PPT presentation

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Title: Drifting Classroom


1
Rivers
2
Discussion Section
  • Referring to your fieldwork results, what type of
    river erosion did you find in your field site?
  • Answer Lateral Erosion - results in widening
    of the valley - removal of material from valley
    walls

3
  • Referring to your fieldwork results, what is the
    direction of river erosion in your field site?
    How does it affect the river channel? Explain
    with an annotated diagram?
  • Answer There are sideway erosion .

4
  • What are the types of river transportation? How
    do you know that they are taking place in your
    site? (Please use fieldwork results to support
    your analysis)
  • Answer Traction . It is because the bed load is
    more heavy which cannot be lifted above the bed.
    Lots of them are pebbles .
  • Saltation . It is because larger particles are
    moved in a series of hops and bounces along the
    river bed .

5
  • What are the characteristics of lower course?
    With the help of fieldwork results, for example
    river width, depth, cross-section, the size of
    bed loads and the nature of stream bed, to prove
    that your site is identified as lower course.
  • Answer

6
  • Compared the width and depth of the channel with
    that of the upper course , the channel of lower
    course accommodates much more water . In my site
    , the width is 7m long and the deepest depth is
    28cm .
  • The channel bed is smoother than the upper course
    .
  • Heavier and angular load has greater potential
    for erosion .
  • A large amount of load , mostly fine and rounded
    .

7
  • What is the feature found at Point A? What other
    feature(s) would be there? Describe and explain
    their formations, illustrate your answer with
    annotated diagrams.
  • Answer We can find waterfall in Point A. In the
    upper course, there are interlocking spurs,
    rapids and potholes.
  • Formation of waterfall River falls vertically
    down and forms waterfalls.
  • Formation of interlocking spurs They are formed
    when the river water is unable to remove the
    obstacles on its path.
  • Formation of rapids The river water is unable to
    erode the layer of resistant rock crossing the
    channel the uneven surface causes turbulent
    currents there. The turbulent currents are called
    rapids.
  • Formation of potholes The water drills hollows
    with the load it carries. The hollow are called
    potholes.

8
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9
  • What is the height difference among Point A, C
    and E? When there is prolonged torrential rain,
    which point(s) will suffer from flooding? Why?
    Suggest sustainable measures to cope with
    flooding.
  • Answer Point A 40 m,
  • Point C 0 m,
  • Point E 0 m.
  • Point E will suffer from flooding .
  • It is because Point E has more tributaries .
  • Suggestion We can build spillways to cope with
    flooding . This helps prevent the discharge to
    rise above the bank full discharge .

10
References
  • http//ihouse.hkedcity.net/hm1203/hydrosphere/riv
    er-work.htm
  • http//www.geography-site.co.uk/pages/revision/riv
    er.html
  • http//facweb.bhc.edu/academics/science/harwoodr/G
    eog102/study/river2.htm
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