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Features Of Erosion
By Jesse, Abdullahi, John, Nderitu
           and Angela.




                                     1
Waterfalls
• Waterfalls are usually
  formed when a river moves
  over resistant bedrock and
  erodes it slowly while
  downstream it happens
  faster.
• As this happens material is
  plucked from a river bed
  which causes the waterfall to
  carve deeper into the
  riverbed and recede
  upstream
• part of the bedrock (hard
  rock) will later break off,
  exposing the soft rock, and
  form a waterfall.
• The rest is in the diagram on
  your right


 6/6/12                           Group Y   2
OX BOW LAKES
•   An ox bow lake is a U - shaped water body or
    meander that is cut of by erosion to form a lake.
•   They are formed when a river has a very curve
    us meander, which is nearly meeting the other
    side of the river.
•   Due to erosion and deposition the neck of the
    meander becomes very narrow which allows
    water to pass straight, flowing past the old
    meander.
•   Deposition then occurs, sealing of the meander.
•   The deposition then totally covers up the
    meander so no more water can pass.
•   Over time the closed meander completely cuts of
    from the rest of the river.
•   The end result is a straight river separated from
    a curved C-shaped lake.


6/6/12                               Group Y            3
OX BOW LAKES




6/6/12        Group Y   4
V-shaped valleys.
•   In the upper course of a river,
    water flows at a high speed
    through a narrow channel with a
    steep gradient.
•   As it does, so it cuts downwards.
•   This vertical erosion results in a
    number of distinctive landforms
    including, the steep sloped v-
    shaped-valleys
•   Through this the river flows in it's
    upper course.




6/6/12                                     Group Y   5
Formation of v-shaped-valleys.
•   Vertical erosion leads to the
    development of steep sided,
    narrow valleys shaped like the
    letter V.
•   The valley sides are steep due to
    the soil and loose rock being
    washed downhill following periods
    of heavy rainfall.
•   The material is then added to the
    load of the river.
•   The river itself forced to wind its
    way through protruding hillsides.
•   These hillsides known as
    interlocking spurs restrict the view
    up or down the valley.


6/6/12                                     Group Y   6
RAPIDS
•   A river rapid is a section of a river
    with a steep gradient, which cases
    an increase in the water velocity
    and the turbulence.
•   A rapid is caused by the river
    becoming shallower and having
    some materials, like rocks, to be
    exposed above the flow surface.
•   In rapids, water turns white
    because flowing water splashes
    over and around the rocks, and air
    bubbles mix with them.
•   This colour is normally called
    “White water”.
•   Rapids normally occur when the
    river bed is highly resistant to
    erosion.

6/6/12                                  Group Y   7
Rapids
•      Rapids are categorized into several
       classes:
•      Class 1- This is when the river has small
       waves in fast flowing water and has very
       few obstacles, e.g. rocks.
•      Class 2- When the river has wide
       channels and rapids , without many
       turns and obstacles.
•      Class 3- This class has strong currents
       with many obstacles in the river.
•      Class 4- Powerful rapids with big waves
•      Class 5-Very violent and dangerous
       rapids with tight turns
•      Class 6- This last stage is the most
       violent and strong. This rapid can cause
       death easily.




    6/6/12                                    Group Y   8
Rapids
•   Many people use these river
    rapids to have fun.
•   Rafting, is a sport which requires
    rapids.
•   Rafting courses are also
    classified using these rapid
    classes.




6/6/12                                   Group Y   9

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Features of erosion

  • 1. Features Of Erosion By Jesse, Abdullahi, John, Nderitu and Angela. 1
  • 2. Waterfalls • Waterfalls are usually formed when a river moves over resistant bedrock and erodes it slowly while downstream it happens faster. • As this happens material is plucked from a river bed which causes the waterfall to carve deeper into the riverbed and recede upstream • part of the bedrock (hard rock) will later break off, exposing the soft rock, and form a waterfall. • The rest is in the diagram on your right 6/6/12 Group Y 2
  • 3. OX BOW LAKES • An ox bow lake is a U - shaped water body or meander that is cut of by erosion to form a lake. • They are formed when a river has a very curve us meander, which is nearly meeting the other side of the river. • Due to erosion and deposition the neck of the meander becomes very narrow which allows water to pass straight, flowing past the old meander. • Deposition then occurs, sealing of the meander. • The deposition then totally covers up the meander so no more water can pass. • Over time the closed meander completely cuts of from the rest of the river. • The end result is a straight river separated from a curved C-shaped lake. 6/6/12 Group Y 3
  • 5. V-shaped valleys. • In the upper course of a river, water flows at a high speed through a narrow channel with a steep gradient. • As it does, so it cuts downwards. • This vertical erosion results in a number of distinctive landforms including, the steep sloped v- shaped-valleys • Through this the river flows in it's upper course. 6/6/12 Group Y 5
  • 6. Formation of v-shaped-valleys. • Vertical erosion leads to the development of steep sided, narrow valleys shaped like the letter V. • The valley sides are steep due to the soil and loose rock being washed downhill following periods of heavy rainfall. • The material is then added to the load of the river. • The river itself forced to wind its way through protruding hillsides. • These hillsides known as interlocking spurs restrict the view up or down the valley. 6/6/12 Group Y 6
  • 7. RAPIDS • A river rapid is a section of a river with a steep gradient, which cases an increase in the water velocity and the turbulence. • A rapid is caused by the river becoming shallower and having some materials, like rocks, to be exposed above the flow surface. • In rapids, water turns white because flowing water splashes over and around the rocks, and air bubbles mix with them. • This colour is normally called “White water”. • Rapids normally occur when the river bed is highly resistant to erosion. 6/6/12 Group Y 7
  • 8. Rapids • Rapids are categorized into several classes: • Class 1- This is when the river has small waves in fast flowing water and has very few obstacles, e.g. rocks. • Class 2- When the river has wide channels and rapids , without many turns and obstacles. • Class 3- This class has strong currents with many obstacles in the river. • Class 4- Powerful rapids with big waves • Class 5-Very violent and dangerous rapids with tight turns • Class 6- This last stage is the most violent and strong. This rapid can cause death easily. 6/6/12 Group Y 8
  • 9. Rapids • Many people use these river rapids to have fun. • Rafting, is a sport which requires rapids. • Rafting courses are also classified using these rapid classes. 6/6/12 Group Y 9