Landforms

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6 Terms

1
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How are waterfalls formed?

  • Drop in the river bed from one level to another due to changes in the hardness of the rock, where hard rock overlies soft rock

  • Hydraulic action and abrasion are the main erosional processes:

  • The soft rock erodes quicker, undercutting the hard rock - creating a plunge pool

  • leads to the development of an overhang of hard rock which eventually collapses

  • overhang falls into the plunge pool increasing abrasion and making the plunge pool deeper

  • process then repeats and the waterfall retreats upstream leaving a steep-sided gorge

<ul><li><p>Drop in the river bed from one level to another due to changes in the hardness of the rock, where hard rock overlies soft rock</p></li><li><p>Hydraulic action and abrasion are the main erosional processes:</p></li><li><p>The soft rock erodes quicker, undercutting the hard rock - creating a plunge pool</p></li><li><p>leads to the development of an overhang of hard rock which eventually collapses</p></li><li><p>overhang falls into the plunge pool increasing abrasion and making the plunge pool deeper</p></li><li><p>process then repeats and the waterfall retreats upstream leaving a steep-sided gorge</p></li></ul>
2
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What is a V-shaped valley, and how does it form?

    - Narrow, steep-sided valley in the upper course.

Formed by:

    - Vertical erosion is dominant in the upper course of the river

  • This cuts down into the river bed and deepens the river channel 

  • Weathering and mass movement lead to material from the valley sides collapsing into the river, forming a steep v-shaped valley


<p>&nbsp; &nbsp; - Narrow, steep-sided valley in the upper course.</p><p>Formed by:</p><p style="text-align: start">&nbsp; &nbsp; - <strong>Vertical erosion</strong> is dominant in the upper course of the river</p><ul><li><p>This cuts down into the river bed and deepens the river channel&nbsp;</p></li></ul><ul><li><p><strong>Weathering</strong> and <strong>mass movement</strong> lead to material from the valley sides collapsing into the river, forming a steep v-shaped valley</p></li></ul><p><br></p>
3
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What are interlocking spurs?

    In lowland areas, lateral erosion is dominant

  • Meanders increase in size

  • The fastest water flow (thalweg) is on the outside of the river bends, leading to erosion:

    • The erosion undercuts the riverbank, forming a river cliff

    • The riverbank collapses and the edge of the meander moves further out

  • The slowest flow is on the inside of the river bends, leading to deposition:

    • The deposits form a slip-off slope

  • Deposition on one side and erosion on the other leads to the meander migrating across the valley

4
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Formation of oxbow lakes

  • With distance downstream, the size of the meanders increases

  • The erosion on outside bends can eventually lead to the formation of a meander neck

  • At a time of the flood, the river may cut through the neck of the meander, forming a straighter course for the water

  • The flow of water at entry and exit from the meander will be slower, leading to deposition

  • The meander becomes cut off from the main river channel, forming an oxbow lake

<ul><li><p>With distance downstream, the size of the meanders increases</p></li><li><p>The erosion on outside bends can eventually lead to the formation of a meander neck</p></li><li><p>At a time of the flood, the river may cut through the neck of the meander, forming a straighter course for the water</p></li><li><p>The flow of water at entry and exit from the meander will be slower, leading to <strong>deposition</strong></p></li><li><p>The meander becomes cut off from the main river channel, forming an <strong>oxbow lake</strong></p></li></ul>
5
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Describe floodplains and levees.

    - Floodplains: Flat land formed by meander migration.

    - Levees: Natural embankments formed by deposition.

6
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What factors influence delta formation?

    - Sediment load, drop in river velocity, flocculation.

    - Bioconstruction (vegetation slowing water).