In a paragraph compare North America and South America focus on physical features

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Answer 1

Answer:

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South America can be divided into three physical regions: mountains and highlands, river basins, and coastal plains. Mountains and coastal plains generally run in a north-south direction, while highlands and river basins generally run in an east-west direction. While North America can be divided into five physical regions: the mountainous west, the Great Plains, the Canadian Shield, the varied eastern region, and the Caribbean. Mexico and Central America's western coast are connected to the mountainous west, while its lowlands and coastal plains extend into the eastern region.

Explanation:

Answer 2

Water, lakes, mountains and deserts are example of physical features found on the Earth's surface. Among these are land forms,climate, soils and animal life.

Mountains and highlands, river basins, and coastal plains are the geographic regions that comprise South America. Mountains and coastal plains flow north to south, whereas high lands and river basins go east to west. The mountainous west, the Great Plains, the Canadian Shied, the diverse eastern area, and the Caribbean are the five physical regions that make up North America. The western coasts of Mexico and Central America are connected to the hilly west, while the lowlands and coastal plains of the east stretch into the region.

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Related Questions

How is an occluded front different from a cold front

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Answer:

A warm air occlusion or occluded front is less common than a cold occlusion. A warm occlusion occurs as cool air moves rapidly into an area with an existing warm front. The difference from a cold occlusion is that the approaching cool air is not as cold as the retreating cold air in the existing front.

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The answer is your second option. As an occluded front passes the air is typically drier. During a cold front, as cool air moves in an area, warm, less dense air is pushed above cooler more dense cold air causing temperatures to be colder near the ground.
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