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Transcription:

Chapter 5 Preview

Section 1 The Land

Objectives Identify some key similarities and differences in the physical geography of the United States and Canada. Explain why rivers have played such an important role in this region s development. Examine geographic factors that have made the United States and Canada so rich in natural resources.

Terms divide headwaters tributary fall line fishery

Landforms The Western Mountains and Plateaus The western mountains of North America are called the Pacific Ranges. They include Alaska s Mount McKinley, the highest point on the continent. The Rocky Mountains link the United States and Canada and stretch northwest from New Mexico to Alaska. Dry basins and plateaus, featuring Death Valley and the Grand Canyon, fill the area between the mountain ranges.

Landforms Interior Landforms East of the Rockies, the land falls and flattens into the Great Plains, which extend across the center of North America.

Landforms Eastern Mountains and Lowlands North America s oldest mountain chain, the Appalachians, extends from Quebec in Canada to Alabama in the United States. The Canadian Shield, a giant core of rock, makes up the eastern half of Canada and the northeastern United States.

Landforms Islands North American islands include Manhattan, home to a major world cultural and financial center, in the northeast. The Hawaiian Islands in the Pacific are volcanic mountaintops. Greenland, the world s largest island, is just off the coast of Canada s Ellesmere Island.

DISCUSSION QUESTION Which areas of the region would you predict are the most densely populated? Why do you think so?

ANSWER People tend to settle near sources of freshwater and in mild climates. Mountaintops are too cold and the deserts are too dry for many people to live there. People would settle in the Great Plains because the farmland is rich and abundant. Some of the islands are probably crowded, as are most coastal areas where large cities are located. Other populated areas border lakes and rivers that serve as transportation arteries.

A Fortune in Water Rivers from the Rockies The high ridge of the Rockies is called the Continental Divide. Water flows west of the Divide toward the Pacific Ocean and east of the Divide into the Mississippi River and the Gulf of Mexico.

A Fortune in Water The Mighty Mississippi One of North America s longest rivers, the Mississippi flows 2,350 miles (3,782 km) from its source. It begins in Minnesota as a stream and ends as a broad river that empties into the Gulf of Mexico. The Mississippi drains all or part of 31 U.S. states and 2 Canadian provinces. It is one of the world s busiest commercial waterways.

A Fortune in Water Eastern Rivers The St. Lawrence, one of Canada s most important rivers, forms part of the United States- Canada border. The Canadian cities of Quebec, Montreal, and Ottawa developed along the St. Lawrence River and its tributaries. Niagara Falls, located on a river connecting Lake Ontario and Lake Erie, is a major source of hydroelectric power for Canada and the United States.

A Fortune in Water From Glaciers to Lakes Glacial dams created Canada s Great Bear Lake and Great Slave Lake. The Great Lakes Lakes Superior, Erie, Michigan, Ontario, and Huron are basins created by glacial activity. The Great Lakes-St. Lawrence Seaway is a network of canals, rivers, and waterways linking the Great Lakes with the Atlantic Ocean.

DISCUSSION QUESTION What is the importance of the Mississippi River in U.S. history and economics? Explain.

ANSWER The river stretches almost the full length of the country s interior, so it provides a means for transporting people and goods. European explorers used the Mississippi to venture into new territories.

Natural Resources Fuels An abundance of resources, such as fossil fuels and minerals, has contributed to the prosperity of the United States and Canada. Minerals Gold, silver, and copper are found in the Rocky Mountains. Nickel and iron are mined in parts of the Canadian Shield. Deposits of low-grade iron ore exist in northern Minnesota and Michigan. Canada supplies much of the world s potash, copper, and silver.

Natural Resources Timber Today forests cover less than 50 percent of Canada and just 30 percent of the United States. Commercial loggers face the challenge of harvesting trees while preserving the remaining forests. Fishing The coastal waters of the Atlantic and Pacific Oceans and the Gulf of Mexico are important sources of fish and other sea animals. Because of overfishing, however, the Grand Banks, off Canada s southeast coast, are now off limits to cod fishers.

SECTION 2 Climate and Vegetation

Objectives List the climate zones found in the United States and Canada. Describe how winds, ocean currents, latitude, and landforms affect the region s climates. Identify the kinds of weather hazards that affect the United States and Canada. Discuss how human settlement has affected the natural vegetation of the United States and Canada.

Terms to Know timberline chinook prairie supercell hurricane blizzard

A Varied Region Two-thirds of Canada and the U.S. state of Alaska experience long, cold winters and brief, mild summers. Most of the continental United States and the southern one-third of Canada enjoy temperate climates, depending on elevation. Hawaii, in the South Pacific, has a tropical climate.

Northern Climates Large parts of Canada and Alaska lie in a subarctic climate zone with very cold winters and extensive coniferous forests. Winter temperatures can fall as low as -70ºF ( 57ºC). Bitter winters and cool summers in the tundra along the Arctic coastline make the area unsuitable for most plants or people. Greenland boasts only a few ice-free areas with some extremely hardy trees.

Western Climates Marine West Coast A marine west coast climate brings nearly 100 inches (254 cm) of rainfall every year to the Pacific coast from California to southern Alaska. This amount of precipitation, combined with cool temperatures, is ideal for coniferous forests, ferns, and mosses.

Western Climates - Plateaus, Basins, and Deserts The region between the Pacific Ranges and the Rocky Mountains includes deserts and steppes. The weather is hot and dry. Cacti and wildflowers bloom during the brief spring rains. Elevation gives the higher reaches of the Rocky Mountains and Pacific Ranges a highlands climate. Beyond the timberline, coniferous forests give way to only lichens and mosses. In the spring, the warm, dry chinook wind thaws the snows at the base of the eastern slopes of the Rockies.

ANSWER At high altitudes, the temperatures are too cold for trees to grow. Soils are generally shallow, rocky, and frozen, so seeds do not germinate.

Interior Climates Prairies Prairies, or naturally treeless expanses of grasses, spread across North America s midsection. Some prairie grasses grow up to 12 feet high (3.7 m) as a result of rainfall ranging from 10 to 30 inches (26 to 76 cm) every year. The Dust Bowl When farmers settled the Great Plains, they plowed up the sod formed by prairie grasses, leaving the soil without protection. During the 1930s, several seasons of drought and dry winds blew the soil away, and the area was nicknamed the Dust Bowl.

Eastern Climates The southeastern United States, with a humid subtropical climate, has mild winters and long, muggy summers. Much of the original deciduous forest has been cleared for agriculture. Wetlands and swamps shelter a great variety of plants and animals. Every summer, the region prepares for hurricanes.

Eastern Climates The northeastern United States and southeastern Canada have a humid continental climate with bands of deciduous and mixed forestland. Much of this area is prone to winter blizzards snowstorms with high winds, heavy or blowing snow, and little visibility.

Tropical Climates Hawaii, Puerto Rico, and the southern tip of Florida have tropical climates. Southern Florida has a tropical savanna area, and both Hawaii and Puerto Rico have tropical rain forests.