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Features
formed by a
river.
Summary
        Year 10 Geography
Features
formed in the
upper course of
a River.
WATERFALLS
WATERFALL FORMATION

 In this world waterfalls are found
  anywhere.
 Rivers or streams run through
  rocky landscapes.
 Waterfalls are also human
  attractions but some times they
  are dangerous.
WATERFALL FORMATION
Where are waterfalls common found?
   Waterfalls are often found on rivers or streams that
    run through rocky landscapes.
   But not just on every landscape the land it should
    have a harder rock overlays a layer of softer rock.




             Harder rock



         Softer rock
Waterfall formation
   As the river continues to passes over the
    sorter rock, it is able to erode the soft rock at a
    faster rate because it is not strong enough to
    hold the volume of the water
   Because of that the soft rock is slowly eaten
    away or eroded forming a curved ledge
    underneath the hard rock.



      Collapsed rocks
 When this happens a plunge pool can
  be formed at the bottom once the
  water had started tumbling down.
 when the water starts tumbling down
  some of the water goes under the
  waterfall and under cuts the soft rock.
 when more of the soft rock is eroded
  there isn’t enough support under the
  harder rock and it collapses into the
  plunger pool.
WATERFALL FORMATION
• The processes of erosion continues further eroding
  the notch and plunge pool.
• The harder rock above will collapse again meaning
  the waterfall will retreat upstream over time and it
  looks like this.
What is a gorge?
   A canyon or gorge is a deep
    ravine between cliffs often
    carved from the landscape by a
    river. Rivers have a natural
    tendency to reach a baseline
    elevation, which is the same
    elevation as the body of water
    it will eventually drain into.
How is a gorge formed?
   Most gorges are formed through
    water erosion. For
    example, waterfalls erode the rocks
    they fall over and the falls move
    gradually back - leaving a gorge
    behind them. Some gorges are formed
    as rift valleys; land stretches and a
    central area drops down - this has
    formed the Great Rift Valley in Africa
    and the Great Glen in Scotland.
Three stages in gorge
formation
               Stage 1




                         Stage 3
 Stage 2
Features formed in
the Middle course
of a River.
Slip off slope
 A slip off slope is formed when the rivers’
  energy is too low. The current is too slow
  when the river energy is low so the river
  cannot carry any load.
 The slip off slope is formed as a result of
  deposition along the river bank. Material
  that was being transported is deposited
  because friction between the water and
  the bank is greater on the inner bank.
Slip off slope
Slip off slope
Meanders
   A meander is a bend in the river, it is
    usually in the lower and middle course of
    the river where the water slides from one
    side of the river to the next, this erodes
    one side of the river bed and deposits
    sediment on the other to make a bend.
How it is formed.

   As water in the
    river flows in the
    middle course of
    the river the
    gradient of the
    river is less steep
    so the river begins
    to meander.
   This is
    because the
    fast flowing
    water on the
    outside of the
    bend erodes
    the side the
    side of the
    river.

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Features formed by rivers

  • 2. Features formed in the upper course of a River.
  • 4. WATERFALL FORMATION  In this world waterfalls are found anywhere.  Rivers or streams run through rocky landscapes.  Waterfalls are also human attractions but some times they are dangerous.
  • 5. WATERFALL FORMATION Where are waterfalls common found?  Waterfalls are often found on rivers or streams that run through rocky landscapes.  But not just on every landscape the land it should have a harder rock overlays a layer of softer rock. Harder rock Softer rock
  • 6. Waterfall formation  As the river continues to passes over the sorter rock, it is able to erode the soft rock at a faster rate because it is not strong enough to hold the volume of the water  Because of that the soft rock is slowly eaten away or eroded forming a curved ledge underneath the hard rock. Collapsed rocks
  • 7.  When this happens a plunge pool can be formed at the bottom once the water had started tumbling down.  when the water starts tumbling down some of the water goes under the waterfall and under cuts the soft rock.  when more of the soft rock is eroded there isn’t enough support under the harder rock and it collapses into the plunger pool.
  • 8. WATERFALL FORMATION • The processes of erosion continues further eroding the notch and plunge pool. • The harder rock above will collapse again meaning the waterfall will retreat upstream over time and it looks like this.
  • 9. What is a gorge?  A canyon or gorge is a deep ravine between cliffs often carved from the landscape by a river. Rivers have a natural tendency to reach a baseline elevation, which is the same elevation as the body of water it will eventually drain into.
  • 10. How is a gorge formed?  Most gorges are formed through water erosion. For example, waterfalls erode the rocks they fall over and the falls move gradually back - leaving a gorge behind them. Some gorges are formed as rift valleys; land stretches and a central area drops down - this has formed the Great Rift Valley in Africa and the Great Glen in Scotland.
  • 11. Three stages in gorge formation Stage 1 Stage 3 Stage 2
  • 12. Features formed in the Middle course of a River.
  • 13. Slip off slope  A slip off slope is formed when the rivers’ energy is too low. The current is too slow when the river energy is low so the river cannot carry any load.  The slip off slope is formed as a result of deposition along the river bank. Material that was being transported is deposited because friction between the water and the bank is greater on the inner bank.
  • 16. Meanders  A meander is a bend in the river, it is usually in the lower and middle course of the river where the water slides from one side of the river to the next, this erodes one side of the river bed and deposits sediment on the other to make a bend.
  • 17. How it is formed.  As water in the river flows in the middle course of the river the gradient of the river is less steep so the river begins to meander.
  • 18. This is because the fast flowing water on the outside of the bend erodes the side the side of the river.