What are the similarities and differences between the terrain of North America and the terrain of So

If you open the topographic map of the world, you can see that the Cordillera Mountains, the longest mountain system in the world, stretches from western North America to western South America (mainly the Rocky Mountains in North America and the Andes Mountains in South America).

So, to put it simply, the common denominator between the two continents is that the west is a tall mountain range.

The difference is that the topography of North America is divided into three north-south vertical belts, with mountains in the west, great plains in the middle, and gentle mountains and plateaus in the east.

The terrain of South America is divided into two large parts, the western part is also a mountain range, but the plains and plateaus to the east of the mountain range are interspersed.

Same:1Topography: high in the west, low in the center 2Species: Mountains, Plateaus, Plains 3West: Alpine.

Different: 1North America: East and Central Longitudinal Fissure Distribution South America: Interphase Distribution.

2.Topography: North America is high in altitude and undulating.

3.The glacial role of North America is significant.

In general, the western part of North and South America is a series of Gouda mountain ranges, much higher than their eastern part.

The form of North America runs from north to south through the high-low-high shape, from west to east is the Rocky Mountains-Great Plains-Labrador Plateau and the Appalachian Mountains;

South America is bordered by the Andes Mountains to the west, and to the east is the Plain de la Plata-Brazilian Altiplano-Amazon-Guiana Altiplan.

There are some middle school atlases that don't give you a picture, so you need to check it yourself.

The terrain of North America is complex and diverse, with mountains and plateaus dominating. The terrain is high in the west and low in the eastDescends in a stepped pattern. There is a huge difference in height and a large regional difference.

North America has a high average altitude and undulating terrain, and the terrain is divided into three north-south longitudinal belts: tall mountains in the west, vast plains in the middle, and gentle highlands in the east.

The eastern mountains and plateaus, north of the St. Lawrence River by the Labrador Plateau and south of the Appalachian Mountains, are high in the south and low in the north, generally at an altitude of 300,500 meters. The Appalachian Mountains have a narrow coastal plain along the Atlantic Ocean on the east side, which gradually descends to meet the central plain on the west side.

The Central Plains, located between the Labrador Plateau-Appalachian Mountains and the Rocky Mountains, stretches from Hudson Bay in the north to the Gulf of Mexico in the south, and runs through the middle of the continent. There are many lakes and rapids in the northern part of the plain, and the southern part is the Mi-Ishbibi River Plain. To the west of the plain is the world-famous Great Plains.

Western mountains and plateaus.

It belongs to the northern section of the Cordillera mountain system, stretching from Alaska to the south of Mexico, mainly including three parallel mountains, the eastern belt is the Rocky Mountains above 2000-3000 meters above sea level, extending 5000 kilometers from north to south, which is an important demarcation line in North America in terms of climate.

The western belt starts from the coastal mountains of the United States in the south and enters the sea in the north, forming the coastal islands of western Canada, with an altitude of 500-1000 meters; The midzone includes the Alaska Mountains in the north, the Coast Mountains in Canada, the Sierra Nevada and Cascade Ridges in the United States, and others. At 6,193 meters above sea level, Mount McKinley in Alaska is the highest peak in North America.

Topographical features of North America:1. The terrain is high from east to west and low in the middle;

2 The topography of North America is distinctly divided into three north-south vertical belts, with tall mountains in the west, vast plains in the center, and gentle mountains and plateaus in the east;

3 Glacial terrain is widely distributed in the northern half of the continent.

The terrain is high in the east and low on all sides.

The western terrain is mountainous.

According to the query question bank questions, the similarity of the topography of North and South America is ( )aThe northern terrain is plain.

b.The eastern terrain is mountainous. c.

The southern terrain is plateau. d.The western terrain is mountainous.

Answer: d, so the similarity is that the western terrain is mountainous.

America is divided into North America and South America, and is located on the east coast of the Pacific Ocean and the west coast of the Atlantic Ocean. The Americas are located in the Western Hemisphere, which is geographically divided into North America, Central America and South America, with 60 ° south latitude, 80 ° north latitude, 30 ° west longitude and 160 ° west longitude, covering an area of 10,000 square kilometers, accounting for the land area of the earth's surface, the Americas region has about 100 million inhabitants, accounting for the total number of human beings. Duansun Ku is the only continent in the Western Hemisphere as a whole.

North America and South America, bounded by the Panama Canal, are collectively known as America, referred to as the Americas, and the Americas are also known as the "New World".

Topographical features of North America: north-south trending mountains are distributed on the east and west sides parallel to the coast, and the great plains are distributed in the center. The average altitude of North America is relatively high, the terrain is undulating, and the terrain is divided into three major north-south tandem zones

The west is a tall mountain system, the center is a vast plain, and the east is a gentle highland.

Topographic characteristics of South America: The terrain can be divided into two longitudinal zones, east and west, that is, narrow mountains (Andes) in the west and plateaus or plains in the east. The plains of South America below 300 meters above sea level account for about 60% of the continent's area, the plateaus, hills and mountains between 300 meters and 3,000 meters above sea level account for about 33% of the continent's area, and the plateaus and mountains above 3,000 meters above sea level account for about 7% of the continent's area.

The average altitude of the whole continent is 600 meters.

1. The characteristics of the terrain are high in the east and west and low in the middle. The topography of North America is clearly divided into three north-south vertical belts, namely the high mountain system in the west, the vast plains in the middle, and the gentle highlands in the east. North America has a high average altitude and undulating terrain.

2. Eastern Mountains and Plateaus: The Labrador Plateau is north of the St. Lawrence River, and the Appalachian Mountains are south of the Apalachian Mountains, with high terrain in the south and low in the north, and the altitude is generally 300-500 meters. The Appalachian Mountains have a narrow coastal plain along the Atlantic Ocean on the east side, which gradually descends to meet the central plain on the west side.

3. The vast plains in the central part are distributed between the western mountains and the eastern highlands, starting from the Arctic Ocean in the north and reaching the Gulf of Mexico in the south, which is a stretch of the North American continent. A vast plain in the middle of the world, with the world's largest group of freshwater lakes – the Great Lakes (Lake Superior, Lake Michigan, Lake Huron, Lake Erie, Lake Ontario).

4. Western Mountains and Plateaus: It belongs to the northern section of the Cordillera mountain system, stretching from Alaska to the south of Mexico, mainly including three parallel mountains, the eastern belt is the Rocky Mountains above 2000-3000 meters above sea level, extending 5000 kilometers from north to south, which is an important demarcation line in the climate of North America; The western belt stretches from the coastal mountains of the United States in the south to the sea in the north, forming the coastal islands of western Canada, with an altitude of 1,000-500 meters: the middle belt includes the Alaska Mountains in the north, the Coast Mountains in Canada, the Sierra Nevada and Cascade Ridges in the United States, etc.