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How were Himalayas formed?

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Anonymous

8y ago
Updated: 10/25/2021

The Himalayas were formed around 70 million years ago, when the Indo-Australian Plate collided with the Eurasian Plate at a convergent/destructive plate boundary. This has caused fold mountains to form as there are no subductions of the plates that can be seen from the absence of volcanoes in the Himalayas.

The Himalayas or Himalaya is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism. The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan. The first three countries having sovereignty over most of the range. Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre (1,500 mi)-long arc. The range varies in width from 400 kilometres (250 mi) in the west to 150 kilometres (93 mi) in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000-3000 m, known as the Lower Himalayan Range.

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Myra Bradtke

Lvl 10
3y ago

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Related Questions

When was the himalayus formed?

when was the Himalayas formed?


The Himalayas were formed at a?

The Himalayas are a mountain range in Asia. They are being formed by the Indian subcontinent submerging under the Asian continent.


What type of plate margin formed the Himalayas?

the Himalayas were formed by a collision plate boundary, meaning that the plates collided and formed the Himalayas. The Himalayas are also referred to as 'fold mountains' because of the way in which they are made.


What type of plates form the Himalayas?

the Himalayas were formed by a collision plate boundary, meaning that the plates collided and formed the Himalayas. The Himalayas are also referred to as 'fold mountains' because of the way in which they are made.


Which mountains were formed when two continents collided?

The most notable are the Himalayas, formed when India (on the Indo-Australian plate) drove north into Asia.


What are mountains formed by the collision of the indo Australian plate and the Eurasian plate?

The Himalayas formed :]


The border between Nepal and Tibet is formed by what mountain?

Mount Everest, which is found in the Himalayas mountain range


What plate margin formed the Himalayas?

The Himalayas were formed at a convergent plate margin where the Indian Plate collided with the Eurasian Plate. This collision resulted in the uplift of the Himalayan mountain range.


How were the Andes mountains the Himalayas and the islands of japan formed alike?

They were all formed at convergent boundaries


How was the mountain system of the Himalayas formed?

the humans of Himalaya built them


What from of plate tectonic movement formed the Himalayas?

The Himalayas were formed by the collision of the Eurasian plate (continental) and the Indo-Australian plate (continental).


What type continental boundary caused the Himalayas to be formed?

The Himalayas were formed by the collision of the Indian Plate with the Eurasian Plate. This is an example of a convergent boundary, where two plates move towards each other, resulting in the uplifting of the Earth's crust and the formation of large mountain ranges.