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The Himalayas are young fold mountains formed by the convergence of two tectonic plates. They constitute one of the 5 physiographic divisions of India. Along with acting as a grand barrier guarding India’s frontiers, they also act as a dividing range between the Tibetan Plateau in the north and India in the south.
NCERT Summary: The Himalayas | Geography for UPSC CSE

Formation of Himalayas

The Himalayas were formed several million years ago as a result of the convergence of the Indo-Australian Tectonic Plate with the Eurasian (Asian) Tectonic Plate. The series of events that led to their genesis and evolution are listed chronologically below:

NCERT Summary: The Himalayas | Geography for UPSC CSE

  1. Pangea and Panthalassa (250 million years ago):
    • Pangea was a supercontinent that existed during the late Paleozoic and early Mesozoic eras. It was surrounded by a vast ocean called Panthalassa.
  2. Breaking of Pangea (150 million years ago):
    • Pangea began to break apart into smaller landmasses, primarily Laurasia (or Angaraland) in the north and Gondwanaland in the south.
    • Laurasia comprised present-day North America, Europe, and Asia, while Gondwanaland included South America, Africa, South India, Australia, and Antarctica.
  3. Formation of Tethys Sea:
    • The breakup of Pangea created a long, narrow sea called the Tethys Sea, situated between Laurasia and Gondwanaland.
  4. Deposition of Sediments:
    • Over time, rivers flowing from both Laurasia and Gondwanaland deposited large amounts of sediment into the Tethys Sea, gradually filling it up.
  5. Breaking Down of Gondwanaland and Angaraland:
    • As the tectonic activity continued, Gondwanaland and Angaraland fragmented further into smaller landmasses.
    • From Gondwanaland, the Indo-Australian Plate emerged, encompassing present-day Australia and the Indian Subcontinent.
    • From Angaraland, the Eurasian Plate emerged, including present-day Europe and Northern Asia.
  6. Convergence of Indo-Australian and Eurasian Plates:
    • Driven by convection currents in the Earth's mantle, the Indo-Australian Plate started to drift northward toward the Eurasian Plate.
    • This movement persisted over millions of years, leading to the eventual convergence of the two plates across the Tethys Sea.
  7. Formation of Folds:
    • As the Indo-Australian Plate continued its northward movement, the area occupied by the Tethys Sea began to shrink.
    • The sediments deposited in the seabed of the Tethys Sea were gradually pushed upwards, resulting in the formation of folds in the Earth's crust.
  8. Genesis of the Himalayas:
    • Eventually, the Tethys Sea vanished entirely as a result of the converging plates and the upward movement of sediments.
    • The sedimentary layers lifted from the former seabed formed a massive mountain range, which we now know as the Himalayas.
  9. Continued Convergence:
    • Presently, the Indo-Australian and Eurasian Plates continue to converge, albeit at a slow pace.
    • This ongoing convergence leads to the gradual upliftment of the Himalayas, with the mountain range rising approximately 5 millimeters per year.

Longitudinal Division of Himalayas

On the basis of the latitudinal extent, the Himalayas can be divided into three divisions:

  1. Trans-Himalayas.
  2. The Himalayan Mountain Ranges.
  3. The Eastern Hills or Purvanchal.

NCERT Summary: The Himalayas | Geography for UPSC CSE

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The Trans-Himalayas 

  • The Trans-Himalayas are the Himalayan Ranges located north of the Great Himalayan Range.
  • They span approximately 1,000 kilometers in an east-west direction.
  • The average elevation of this region is around 3,000 meters above mean sea level.
  • Prominent ranges within the Trans-Himalayas include the Karakoram Range, the Ladakh Range, and the Zaskar Range.

Karakoram Range

  • The Karakoram Range is the northernmost part of the Trans-Himalayas in India.
  • It serves as the boundary between India and Afghanistan as well as China.
  • With an average width of 110-130 kilometers, it boasts some of the world's highest peaks and largest glaciers.
  • Notable features include K2 (Mount Godwin-Austen), the world's second-highest peak at approximately 8,611 meters, and glaciers like the Siachen Glacier and Remo Glacier.

Ladakh Range


  • The Ladakh Range is seen as an extension of the Karakoram Range towards the southeast.
  • It stretches from the mouth of the Shyok River in North Kashmir towards the Indo-Tibetan borders.
  • Occasionally, the Deosai Mountains in Pakistan-Occupied Kashmir (POK) and the Kailash Range in western Tibet are considered part of the Ladakh Range.

Zaskar Range

  • The Zaskar Range runs roughly parallel to the Great Himalayan Range.
  • Extending southeast from the Suru River to the upper Karnali River, it is characterized by its own unique features.
  • The highest peak in this range is Kamet Peak, standing at 25,446 feet.

The Himalayan Ranges

  • Composition: The Himalayan Range, the youngest mountain range globally, is primarily composed of uplifted sedimentary and metamorphic rocks.
  • Boundaries
    • Bordered to the northwest by the Karakoram and Hindu Kush ranges, to the north by the Tibetan Plateau, and to the south by the Indo-Gangetic Plains.
    • While the southern boundary is well-defined by foothills, the northern boundary blends into the edge of the Tibetan Plateau.
  • Extent: Spans over 2,400 kilometers from the Indus Gorge in the west to the Brahmaputra Gorge in the east.
  • Width: Wider in the western side compared to the eastern side.
  • Elevation:
    • Average elevation approximately 6,100 meters.
    • Western Himalayas show gradual elevation change, while the Eastern Himalayas exhibit rapid elevation changes.

Greater Himalayas (Himadri)


  • Also known as Inner Himalayas or Central Himalayas.
  • Composed of ancient rocks like granite, gneisses, and schist.
  • Orientation varies across regions:
    • Extends southeast across northern Pakistan, India, and Nepal.
    • Curves eastwards across Sikkim and Bhutan.
    • Turns northeast across northern Arunachal Pradesh.
  • Home to world's highest peaks including Nanga Parbat, Mount Everest, Kanchenjunga, and Namcha Barwa.
  • Slopes steep towards the north and gentle towards the south.

Inner or Middle Himalayas

  • Also termed Lesser or Lower Himalayas.
  • Mean elevation 3,500 to 5,000 meters, average width 60 to 80 kilometers.
  • Prominent ranges: Nag Tibba, Mahabharat Range, Dhauladhar, Pir Panjal, and Mussoorie Range.
  • Important rivers like Jhelum and Chenab traverse this region.
  • Famous Valley of Kashmir lies between Pir Panjal and Zanskar range.
  • Hosts hill resorts like Shimla, Chail, Ranikhet, Nainital, Almora.
  • Formation of Karewas, fluvioglacial deposits, is notable.
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Shiwalik or Outer Himalayas

  • Southernmost range, lying between Middle Himalayas in the north and Indo-Gangetic Plains in the south.
  • Rises abruptly from Indus and Ganges plains in the south, parallel to the main Himalayan Range in the north.
  • Separated from the main range by valleys.
  • Churia Range in Nepal.
  • Formation of Doons and Duars: Upliftments halted river flow, forming temporary lakes. Sediments deposited formed fertile alluvial soils, known as Doons in the west and Duars in the east, vital for tea cultivation.

NCERT Summary: The Himalayas | Geography for UPSC CSE

The Eastern Hills or the Purvanchal


  • The Himalayas take a sudden southward turn near the Dihang Gorge due to the Syntaxial Bend, giving rise to a series of relatively low hills known as the Purvanchal or Eastern Hills.
  • Extending from Arunachal Pradesh in the north to Mizoram in the south, these hills serve as India’s border with Myanmar.

Prominent Ranges:

  • Patkai Bum: Located along the boundary between Arunachal Pradesh and Myanmar, the Patkai Bum is the northernmost range of the Purvanchal.
  • Naga Hills: South of Patkai Bum, the Naga Hills, along with Patkai Bum, form the watershed between India and Myanmar.
  • Manipur Hills: Situated south of the Naga Hills, the Manipur Hills are separated from the Naga Hills by the Barail Range.
  • Mizo Hills or Lushai Hills: Found to the south of the Manipur Hills, the Mizo Hills or Lushai Hills complete the series of hills in the Purvanchal region.

NCERT Summary: The Himalayas | Geography for UPSC CSE

Regional Division of Himalayas

Based on the longitudinal extent, the Himalayas have been divided into 4 regional divisions – Punjab Himalayas, Kumaon Himalayas, Nepal Himalayas, and Assam Himalayas.

Punjab Himalayas:

  • Located between the Indus River in the west and the Sutlej River in the east.
  • Predominantly situated in Jammu and Kashmir and Himachal Pradesh, also known as Kashmir and Himachal Himalayas.
  • Features prominent ranges like Karakoram, Pir Panjal, Ladakh, Zanskar, and Dhauladhar.
  • Characterized by high snow-covered mountains, deep gorges, and mountain passes.

Kumaon Himalayas:

  • Lies between the Satluj River in the west and the Kali River in the east, also known as Garhwal Himalayas in the west.
  • More elevated than the Kashmir Himalayas.
  • Home to notable peaks such as Nanda Devi, Trisul, Kedarnath, and Kamet.
  • Hosts popular hill stations like Nainital, Ranikhet, and Almora.

Nepal Himalayas:

  • Extends from the Kali River in the west to the Tista River in the east, primarily in Nepal.
  • Known for tallest peaks like Mount Everest, Kanchenjunga, and Dhaulagiri.
  • Kathmandu Valley is a prominent feature of this region.

Assam Himalayas:

  • Stretches from the Tista River in the west to the Brahmaputra River in the east, covering Assam and Arunachal Pradesh in India.
  • Lower in elevation compared to Nepal Himalayas.
  • Ranges arranged in a north-south direction due to a sudden southward turn in Arunachal Pradesh.
  • Notable peaks include Namcha Barwa, Gyala Peri, Kengto, and Nyegyi Kangsang.
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Syntaxial Bends of Himalayas

NCERT Summary: The Himalayas | Geography for UPSC CSE

Western Syntaxial Bend:
  • Occurs near Nanga Parbat where the Indus River cuts a deep gorge.
  • Represents the termination of the east-west trend of the Himalayan Ranges.
Eastern Syntaxial Bend:
  • Occurs near Namcha Barwa in Arunachal Pradesh where the ranges turn southwards after crossing the Brahmaputra River.
  • Marks the eastern extremity of the Himalayas.

Significance of the Himalayas

  • Climatic Influence: Himalayas affect India's climate by intercepting monsoonal winds and regulating precipitation.
  • Security: They serve as a natural defense barrier for India.
  • Perennial Source of Water: Source of major rivers in North India.
  • Forest Wealth: Rich biodiversity and raw materials for industries.
  • Agriculture: Terraced slopes support cultivation.
  • Minerals: Abundance of valuable minerals.
  • Hydroelectricity: Potential for hydroelectric power generation due to fast-flowing rivers and rugged topography.


The document NCERT Summary: The Himalayas | Geography for UPSC CSE is a part of the UPSC Course Geography for UPSC CSE.
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FAQs on NCERT Summary: The Himalayas - Geography for UPSC CSE

1. What is the formation process of the Himalayas?
Ans. The Himalayas were formed due to the collision of the Indian Plate with the Eurasian Plate, resulting in the upliftment of the landmass and the formation of the mountain ranges.
2. What are the different divisions of the Himalayas based on their longitudinal extent?
Ans. The Himalayas are divided into the Trans-Himalayas, the Himalayan Ranges, and the Eastern Hills or the Purvanchal based on their longitudinal extent.
3. What is the significance of the Himalayas?
Ans. The Himalayas act as a natural barrier protecting the Indian subcontinent from cold winds, play a crucial role in the monsoon system, and are a source of various rivers that provide water for agriculture and other activities.
4. What are the Syntaxial Bends of the Himalayas?
Ans. The Syntaxial Bends of the Himalayas refer to the sharp bends or curves in the mountain ranges caused by the complex tectonic movements in the region.
5. What are the differences between the Inner Himalayas and the Shiwalik or Outer Himalayas?
Ans. The Inner Himalayas are higher in altitude and consist of snow-capped peaks, while the Shiwalik or Outer Himalayas are lower in altitude and consist of foothills with lesser elevation.
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