Key idea: ice is a powerful force in shaping the land as a result of weathering, erosion, transport and deposition
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 ?
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
1. Draw labelled diagrams to show how each of the following processes operates:
Freeze thaw weathering
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.