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Answer: Glaciers shape the land through processes of erosion, weathering, transportation and deposition, creating distinct landforms.
Glacial processes – shaping the land
Glaciers shape the land through processes of erosion , weathering , transportation and deposition , creating distinct landforms.
Glaciers form when more snow falls than melts each year. Over many years, layer upon layer of snow compacts and turns to ice. There are two different types of glaciers: continental glaciers and valley glaciers. Each type forms some unique features through erosion and deposition.
How do glaciers cause deposition? Glacial deposition occurs when glaciers retreat, leaving behind rocks and soil known as till.
How do glaciers cause erosion and deposition? Process when a glacier drags rocks with it across the land and it gouges and scratches the bedrock. When a glacier melts it deposits the sediment it eroded from land, creating various landforms.
Where and how do glaciers form? Glaciers form in places where more snow falls than melts or sublimates. As the layers of snow pile up, the weight on the underlying snow increases. Eventually, this weight packs the snow so tightly that glacial ice is formed.
Even at high latitudes, glacier formation is not inevitable. Areas of the Arctic, such as Banks Island, and the McMurdo Dry Valleys in Antarctica are considered polar deserts where glaciers cannot form because they receive little snowfall despite the bitter cold.
Glacial tills can include rock flour, clay, silt, sand, gravel, cobbles and boulders depending on the source rock, the mode of deformation, the mode and distance of transportation and the mode of deposition.
Till deposits
Drumlins are oval hills which form in groups called swarms. The unsorted till appears moulded by ice to form a blunt end with a more streamlined, gentler lee slope. Moraines are mounds of poorly sorted till where rock debris has been dumped by melting ice or pushed by moving ice.
A moraine is sediment deposited by a glacier. A ground moraine is a thick layer of sediments left behind by a retreating glacier. An end moraine is a low ridge of sediments deposited at the end of the glacier.