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Glaciation 3
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Glaciation 3

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Glaciation 3 Glaciation 3 Presentation Transcript

  • Key idea: ice is a powerful force in shaping the land as a result of weathering, erosion, transport and deposition
  • Objectives
    • Freeze thaw weathering
    • Processes of erosion - plucking and abrasion
    • Processes of movement and transportation – rotational slip and bulldozing
    • Deposition and the reasons for it
  • Freeze thaw weathering Freeze-thaw is when meltwater or rain gets into cracks in the bed rock, usually the backwall. At night the water freezes, expands and causes the crack to get larger. Eventually the rock will break away
  • Erosion – where rocks are broken down and moved away by ice eg. plucking + abrasion. Weathering - where rocks are broken down ‘in situ’ but are not moved away by ice, water or wind. eg. frost shattering. What is the difference between erosion and weathering ?
  • Glacial Erosion
    • There are two main types of glacial erosion – plucking and abrasion
    • Plucking is the tearing away of blocks of rocks as a glacier moves. These blocks of rock had been frozen to the bottom of the glacier where water had entered joints in the rock and become frozen. When the ice moves downhill, rock is plucked from the back wall.
  • Abrasion is when rock fragments which have frozen to the base and the back of the glacier scrape the bed rock as the ice moves. Smaller rock particles have a sandpaper effect on the rocks over which the ice passes while the sharp edges of large rocks make deep grooves called striations
  • Direction of flow Crevasses
  • Tasks
    • 1. Draw labelled diagrams to show how each of the following processes operates:
        • Freeze thaw weathering
        • Plucking
        • Abrasion
    • 2. Explain why the breakdown and removal of rock is quicker when
        • all three processes operate in the same area
        • Rocks have many lines of weakness
  • Processes of transportation and deposition
    • Moraine is angular rock material which is transported and later deposited by a glacier.
    • It is deposited when there is a rise in temperature.
    • As the glacier begins to melt it cannot carry as much material
  •  
  • Types of moraine
    • Lateral moraine – material derived from freeze-thaw weathering of valley sides and which is carried at the sides of a glacier.
    • Medial moraine – found in the centre of a glacier and results from two lateral moraines joining together.
    • Ground moraine is material dragged underneath a glacier.
    • Terminal moraine – marks the maximum advance of a glacier. It is the rock material deposited at the snout of a glacier.
    • Recessional moraines – these form behind and parallel to the terminal moraine. They mark stages in the retreat of a glacier when it remained stationary for long enough for a ridge of material to develop.
  •