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Formation, Age, and Composition

Geological Age

  1. The Himalayas are young fold mountains, evidenced by:
    • Deep gorges
    • U-turn river courses
    • Parallel ranges
    • Steep gradients
    • Landslides
  2. Relative Age of Ranges:
    • The Shiwalik Range (Outer Himalayas) is the youngest mountain range in India.
    • The Great Himalayan Range is the oldest among the parallel fold ranges.
  3. Geological Eras:
    • The Shiwalik series of rocks was formed in the Cenozoic era.
    • Among Indian rock systems, the Gondwana system is younger than the Vindhyan, Cuddapah, and Dharwar systems.

Rock Composition and Fossils

  • The sedimentary rocks of the Greater Himalayas are fossil-less.
  • The sedimentary rocks of the Lesser Himalayas contain marine living fossils.
  • Remains of human civilization are found in the Outer or Shiwalik Himalayas.

Physiographic Divisions of the Himalayas

Major Parallel Ranges (North to South)

  1. Great Himalayas (Himadri): Oldest and highest range.
  2. Lesser Himalayas: Located between the Shiwalik and the Great Himalayas.
  3. Shiwalik Range: Southernmost and youngest foothills region.

Regional Divisions (West to East)

  • Kashmir Himalaya: Where the ‘Karewa’ landform is found.
  • Kumaon Himalaya: Situated between the Satluj and Kali rivers.

Specific Relief Feature Sequences

  • South to North Sequence 1: Pir Panjal Range → Zaskar Range → Ladakh Range → Karakoram Range.
  • South to North Sequence 2: Dhauladhar Range (Lesser Himalaya) → Zaskar Range → Ladakh Range → Karakoram Range.
  • Mountain Peaks (East to West): Kanchenjunga → Everest → Dhaulagiri → Annapurna.

General Features

  • The Himalayas are spread over more than five Indian states.
  • The altitude of Shiwalik peaks is generally between 850 – 1200 meters.
  • The tree-line in the western Himalayas is at a higher altitude compared to the eastern Himalayas.
  • The height of the Great Himalayas is approximately 8,850 meters above sea level.
  • “Himachal” refers to the Middle Himalaya range.
  • Factors affecting vegetation change with altitude: Decrease in temperature, changes in rainfall, and strong winds.

Associated Landforms

Sub-Himalayan Flat Plains

  • The flat plains along the sub-Himalayan region are called Bhabar.
  • The Bhabar region is an example of a Piedmont situation (a plain at the base of mountains).

Characteristics of Himalayan Rivers

  • Rivers originating from the Himalayas are perennial (flow year-round).
  • This is due to precipitation from both the South-Western monsoon and winter snow, ensuring a continuous water supply.

Eastern Hills and Specific Ranges

Patkai Range

  • It is one of the latest mountain ranges in origin.
  • Indian states along the Patkai hills: Nagaland, Manipur, and Mizoram. Tripura is not situated along the Patkai hills.

Hill Ranges of Meghalaya (West-to-East Sequence)

  • Correct sequence: Garo → Khasi → Jaintia.

Location of Important Places

  • Cherrapunji is situated on the Khasi Hills.
  • The Valley of Kashmir is situated between the Great Himalayas and the Pir Panjal range.
  • Mount Kailash is situated in Tibet.

State-wise Locations of Hills

  • Garo Hills: Meghalaya
  • Miri Hills: Arunachal Pradesh
  • Kollai Mallai Hills: Tamil Nadu
  • Dalma Hills: Jharkhand

Specific Regions and Features

Ladakh Plateau

  • It is a part of the Aksai Chin region.

Western Himalayan Resource Region

  • Its main resources are forests.

Atal Tunnel

  • Built by the Border Roads Organisation (BRO).
  • Connects Manali to Lahaul-Spiti Valley.
  • Strategically important for India.
  • (Note: The data indicates it is not located across the Pir Panjal Range).

Other Indian Geographical Features

Western Ghats

  • They are spread over more than five Indian states.

Pulicat Lake

  • It is spread over two states only (Andhra Pradesh and Tamil Nadu).

Geographical Extent

  • The Himalayan Mountain Ranges are not a part of the state of Uttar Pradesh (the plains of Uttar Pradesh are south of the Himalayas).

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