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NORTH AMERICA
Physiography:  The physiography of North America can be broadly classified into the following divisions: ,[object Object]
Eastern Mountains
Western Mountains
Interior Lowlands & Great Plain
Coastal Plains
Deserts,[object Object]
Canadian Shield: Also known as Laurentian Plateau, or Bouclier canadien in French.  It is basically a basement rock covered by very thin soil. There are several bare rock outcrops dotted with numerous glacial lakes.  The shield has been glaciated many times and the sediment has been carried into the interior lowlands.
The soils in the states of Ohio, Indiana, Iowa, and Illinois are the transported materials from the Canadian shield.   The shield is primarily made up of metamorphic rocks. The shield was originally a region of very large mountains and some volcanic activity, but over the millennia the area was eroded.  The glacial activity over here is quite pronounced and presently this area is covered  by coniferous trees.
The height of the shield ranges from 305m to 610m. There are a number of mountain ranges within the shield: the Adirondack (northeastern New York state), Superior Highlands (northern Minnesota, Wisconsin & Michigan states), Torngat and Laurentian. The shield is a rich source of metallic minerals such as iron, nickel, copper, zinc, uranium, gold, silver, platinum and molybdenum.
This is the highest point of the Canadian Shield Mount Caubvick (1652 m). It is situated in New Foundland.
The Eastern Mountains The eastern mountain complex consist of the Appalachian Mountains. The Appalachians, are about 1,500 miles in length, and 480 km wide extending  from central Alabama in the U.S. up through the New England states and the Canadian provinces of New Brunswick, Newfoundland and Quebec. 
Significant Appalachian ranges include: ,[object Object]
The Blue Ridge Mts. in Virginia
The Alleghenies in Pennsylvania
The Catskills Mts. in New York
The Green Mts. in Vermont
The White Mts. of New HampshireThe highest point is Mt. Mitchell in North Carolina at 6,684 ft (2,037 m) 
The Appalachians are the product tectonic collision. During the middle Ordovician Period (about 496-440 million years ago), a change in plate motions set the stage for the first Paleozoic mountain building event . There were four such tectonic movements which is believed to be responsible for the formation of Appalachian Mountains. At one time the mountains may have been 20,000 feet high. However, today the average height of the Appalachian mountains is 3000ft. Because of dense forests and rugged steep slopes  it acted as a barrier for the first 150 years of European settlement.
The western mountains The western mountain complex consists of mountains, plateaus & valleys. The whole complex can be divided into: ,[object Object]
Intermountain Plateaus
Pacific Mountains and valleys.,[object Object]
Topographically, the Rockies are usually divided into five sections:  ,[object Object]
 The Middle Rockies,
 The Northern Rockies (all in the United States),
 The Rocky Mountain of Canada (Canadian Rockies)The highest point of Canadian Rockies is Mount Robson, 3954m. ,[object Object],*(Many do not consider the Brooks Range to be part of the Rockies) The Wyoming Basin, the system's principal topographic break, is sometimes considered a sixth section.
The plateaus of Western mountain ,[object Object]
The Colorado Rivers drains the 90% of the plateau that carved the beautiful Grand Canyon.,[object Object]

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North America's Diverse Physiography

  • 2.
  • 5. Interior Lowlands & Great Plain
  • 7.
  • 8. Canadian Shield: Also known as Laurentian Plateau, or Bouclier canadien in French. It is basically a basement rock covered by very thin soil. There are several bare rock outcrops dotted with numerous glacial lakes. The shield has been glaciated many times and the sediment has been carried into the interior lowlands.
  • 9. The soils in the states of Ohio, Indiana, Iowa, and Illinois are the transported materials from the Canadian shield. The shield is primarily made up of metamorphic rocks. The shield was originally a region of very large mountains and some volcanic activity, but over the millennia the area was eroded. The glacial activity over here is quite pronounced and presently this area is covered by coniferous trees.
  • 10. The height of the shield ranges from 305m to 610m. There are a number of mountain ranges within the shield: the Adirondack (northeastern New York state), Superior Highlands (northern Minnesota, Wisconsin & Michigan states), Torngat and Laurentian. The shield is a rich source of metallic minerals such as iron, nickel, copper, zinc, uranium, gold, silver, platinum and molybdenum.
  • 11. This is the highest point of the Canadian Shield Mount Caubvick (1652 m). It is situated in New Foundland.
  • 12. The Eastern Mountains The eastern mountain complex consist of the Appalachian Mountains. The Appalachians, are about 1,500 miles in length, and 480 km wide extending from central Alabama in the U.S. up through the New England states and the Canadian provinces of New Brunswick, Newfoundland and Quebec. 
  • 13.
  • 14. The Blue Ridge Mts. in Virginia
  • 15. The Alleghenies in Pennsylvania
  • 16. The Catskills Mts. in New York
  • 17. The Green Mts. in Vermont
  • 18. The White Mts. of New HampshireThe highest point is Mt. Mitchell in North Carolina at 6,684 ft (2,037 m) 
  • 19. The Appalachians are the product tectonic collision. During the middle Ordovician Period (about 496-440 million years ago), a change in plate motions set the stage for the first Paleozoic mountain building event . There were four such tectonic movements which is believed to be responsible for the formation of Appalachian Mountains. At one time the mountains may have been 20,000 feet high. However, today the average height of the Appalachian mountains is 3000ft. Because of dense forests and rugged steep slopes it acted as a barrier for the first 150 years of European settlement.
  • 20.
  • 22.
  • 23.
  • 24. The Middle Rockies,
  • 25. The Northern Rockies (all in the United States),
  • 26.
  • 27.
  • 28.
  • 30. Average Depth: 1600 m
  • 31.
  • 33.
  • 34.
  • 39.
  • 40. The Pacific Coast Range It is a series of mountain range stretching from Alaska to Central Mexico. The Canadian Section of this coast range is called the Canadian Cordilleras.
  • 41.
  • 42. Coast range (Mount Waddington, 4019)
  • 43. Insular Mountain , Vancouver (Golden Hinde, 2196m)
  • 44. Olympic Mountain, (Mt. Olympus, 2427m)
  • 45. Cascade Range (Mt. Rainier, 4392m)
  • 46. Oregon Coast range (Mary’s Peak, 1250m)
  • 48.
  • 49. Great Plains It lies in the eastern side of the Rockies, stretching from Texas to Arctic region of Canada. Some considers it beyond the Rio Grande river in Mexico. It is around 3200 km long and 800 km wide. The Canadian section is often known as Prairies. One of the important rivers of this area is Missouri.
  • 50.
  • 51.
  • 52. The Gulf Coastal Plains The included states are Texas, Louisiana, Alabama, Mississippi and Florida. There are 15 metropolitan areas within the gulf coast region.
  • 53. The Atlantic Coastal Plains consisting off Georgia, North and South Carolina , Virginia up to Boston.
  • 54. Deserts Great Basin Desert Mojave Desert Chihuahuan desert Sonoran Desert (largest)