Features of the Eurasian landform, its development

1. How does the relief of Eurasia differ from the relief of other continents?

In Eurasia, as on all other continents, there are mountains and plains. Here are the highest mountains and the most extensive plains. From the plains and plateaus of North and Central Asia, the peninsulas of the South-West, South and South-East Eurasia are separated by a belt of high mountain systems located in the Alpine-Himalayan folding region. The east of the mainland is framed by a zone

Pacific folding along which mountain systems are also located, the height is much lower than the mountains of the Alpine-Himalayan system.

2. In nature, many processes are not isolated, but in a relationship. How are the areas of earthquakes, volcanoes and mountain building related to each other?

In nature, all processes are interrelated. The development of the earth’s crust is associated with processes of magma displacement occurring in the lower layers of the lithosphere. Internal processes are reflected in external mountain-building processes. In areas of mountain building, earthquakes are frequent, volcanism is intensely manifested. Gaps and discharges of significant parts of the Earth’s surface occur, dips and cracks are formed, which can serve as natural exits to the surface of incandescent magma in the lower layers of the lithosphere under high pressure.

3. What factors can prove that the Eurasian landscape is developing at the present time?

Destructive earthquakes and volcanism, taking away a large number of human lives, are proof that the formation of folded and mobile belts is not completed and is continuing at the present time.

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Features of the Eurasian landform, its development