Vincent Massey Junior High School

Unit 4: Planet Earth

Topic 1

Minerals

Topic 2

Rocks

Topic 3

Erosion and landforms

postcard

Topic 6

Volcanoes

Topic 5

Earthquakes

Faults

Topic 7

Mountains

Topic 4

Moving Crust

Topic 8

Fossils

Topic 9

Geologic Time

Topic 10

Fossil Fuels Geology of Calgary

Topic 3: Erosion

"Big Rock" at Okatoks is a glacial erratic(boulder) left following retreat of
the last ice age 10,000 years ago.

  • students will understand the process of erosion and weathering
  • students will appreciate the effects of erosion on the landscape in which they live.

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

 

 

 

 

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

  • gravity: rocks roll down a slope and break apart
  • rocks in a fast moving stream bump against each other and become smooth and round.
  • temperature change - during the spring snow melts during the day and freezes at night (freeze-thaw). The melt water seeps into rock cracks and expand when the temperature falls below zero. Each freeze-thaw action causes the crack to widen until eventually a piece of rock breaks apart.

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.

Resources: Text Book pages 352-441

 

Morley Bow Valley, Alberta (along Highway 1 between Calgary and Banff)

Glaciers and Moraines


 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Postcard from the Earth's Crust in Canada

Research one of the following land forms, or one that you choose for yourself.

You will need to research the landform from one of the above sites, but you will also need to research HOW that landform was formed. Use a search engine e.g.

Develop a post card on the paper provided the you could send to a friend

On the postcard:

  • Describe where the landform is - country etc (2pts)
  • Describe features - what it looks like, size, shape, materials (5 pts)
  • Describe how it is FORMED (type of weathering) (5pts)
  • All information and picture must go on one side. You may construct this on computer software if you wish.
  • Mount or print card (5 pts)

Mount the picture and information on the paper provided or produce a computer generated postcard.

Be sure that someone else has proof read your card before you hand it in.

Resource: Name of source(s).

Evaluation:

Card
/12
Presentation (appeal/spelling/content
/5
Resources
/2
Marked by:
/1
Total
/20

 

 

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© Diane Nowlan, February 2002

jdnowlan@cbe.ab.ca

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 


 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

All contents copyright © 2002, Diane Nowlan
Revised:January, 2002
Author: Diane Nowlan
jdnowlan@cbe.ab.ca