Question

1) How was Himalayan mountain formed?
2) Explain the features of the great Himalayas.
3) Describe the continental drift theory.
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Answer 1

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How was Himalayan mountain formed?

➡ The Himalayas were formed as a result of the collision between the Indian Plate and Eurasian Plate. As a result of this collision, the sedimentary rocks which were settled in the large-scale depression in the Earth's crust called Tethys were folded and formed the Himalayas.

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Explain the features of the great Himalayas.

➡ The most characteristic features of the Himalayas are their soaring heights, steep-sided jagged peaks, valley and alpine glaciers often of stupendous size, topography deeply cut by erosion, seemingly unfathomable river gorges, complex geologic structure, and series of elevational belts (or zones) that display different.

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Describe the continental drift theory.

➡ Continental drift was a theory that explained how continents shift position on Earth's surface. Set forth in 1912 by Alfred Wegener, a geophysicist and meteorologist, continental drift also explained why look-alike animal and plant fossils, and similar rock formations, are found on different continents.

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Answer 2

Answer:

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Explanation:

➡ The Himalayas were formed as a result of the collision between the Indian Plate and Eurasian Plate. As a result of this collision, the sedimentary rocks which were settled in the large-scale depression in the Earth's crust called Tethys were folded and formed the Himalayas.

______________________

Explain the features of the great Himalayas.

➡ The most characteristic features of the Himalayas are their soaring heights, steep-sided jagged peaks, valley and alpine glaciers often of stupendous size, topography deeply cut by erosion, seemingly unfathomable river gorges, complex geologic structure, and series of elevational belts (or zones) that display different.

______________________

Describe the continental drift theory.

➡ Continental drift was a theory that explained how continents shift position on Earth's surface. Set forth in 1912 by Alfred Wegener, a geophysicist and meteorologist, continental drift also explained why look-alike animal and plant fossils, and similar rock formations, are found on different continents.