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Topic 3: Erosion
"Big Rock" at Okatoks
is a glacial erratic(boulder) left following retreat of
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Dates to Remember April 5 : Weathering and erosion video April 8 : Erosion worksheet due April 9: Landforms project - research April 15: Landforms postcard due. April 15: Rock Cycle presentation due - NO LATES
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New words: Erosion: is the movement of rock and mineral grains from one place to another. Sediments: are the grains that come from larger rocks that have broken down or have been worn away. Weathering: the mechanical, chemical or biological breakdown of rocks. Mechanical weathering: is the physical breakdown or disintegration of rocks e.g
Frost wedging: the freeze thaw process during mechanical weathering. Sedimentation: the build up of weathered material. Chemical weathering: the break down of minerals through chemical reaction such as acid rain (sulphur dioxide and other pollutants that are dissolved in the rain). Biological weathering: is the physical or chemical break down of minerals caused by living organisms such as plants or animals. Physical weathering occurs when plant roots expand in cracks in the rock. Acidic fluids (pee) from animals can cause chemical reactions. Abrasion: wearing down of rocks by wind, fast moving water or ice action. Moraines: piles of sediments that have been push aside or deposited by the melt waters from ice sheets or glaciers. Drumlins: egg-shaped mounds left under the ice sheet by the meltwater as the glacier retreats. Look out for drumlins on the right side of the road at Morley on your next drive to Banff or Kananaskas.
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Resources: Text Book pages 352-441
Morley Bow Valley, Alberta (along Highway 1 between Calgary and Banff) Glaciers and Moraines
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Postcard from the Earth's Crust in Canada |
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© Diane Nowlan, February 2002
All contents copyright © 2002, Diane Nowlan
Revised:January, 2002
Author: Diane Nowlan
jdnowlan@cbe.ab.ca