Convection in the mantle and pressure of magma on the edge of the plate
Explanation:
Convection currents occur in the mantle because the upper mantle (asthenosphere) is generally cooler than the lower mantle. The convections apply upward pressure on the lower edges on the lithosphere as the melted rocks upwell from below. The lithosphere deflects the convections and as the convections churn clockwise of anticlockwise, they drag the lithosphere with it via friction. This is what is stipulated to cause tectonic plate movements.
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Answer:
mongolia
Explanation:
Mongolia has very little arable land, which means historically they have not been able to grow enough crops to support a large population. Until the 20th century Mongolians were largely a herding people, and that just doesn't support dense populations.
Answer:
banff national park
mountain recreation and galcial lakes
Answer:
<u>North Atlantic Ocean</u>
Explanation:
- Gulf stream that forms the extension of the North Atlantic drift and is a warm ocean current that stretches through the tip of Florida and flows through the eastern coast of the United States and reaches the Newfoundlands before crossing the Atlantic ocean and is known to reach the Mexican gulf also.
- At 40°0′N 30°0′W, it separated into two streams as a northern stream, the North Atlantic Drift, and hence influence the climates of the eastern coast of North America and the climates of western Europe.
- This steam typically stretches from 100 kilometers and is 3,900 ft deep. And stream carries warm waters across Atlantic and this is a reason for the intensity of cyclones.
