Great Indian Plains: Regional Division

Trans Gangetic Plains

  1. Rajasthan Plain
    • Rajasthan plain borders the Thar desert (called Marusthali) in the west and Aravallis in the east.
    • This plain is an undulating plain (wave-like) whose average elevation is about 325 m above mean sea level.
    • The eastern part of Marusthali is rocky and the western part is covered by shifting sand dunes called Dhrian.
    • The region receives a rainfall of 25cm.
    • It is spread over Gujarat, Rajasthan, and Punjab.
    • One of the major inland rivers in the region is Luni which drains into the Rann of Kutch region.
    • The irrigation system in the region is the Indira Gandhi Canal.
    • Salination of Lakes in the Region
      • Major saline lakes are Sambhar, Didwana, Degana, Kuchaman, etc. The largest is the Sambhar lake near Jaipur.
      • The reason for salination is the high evaporation rates.
  2. Punjab – Haryana Plain
    • This plain is formed by five important rivers of the Indus system.
    • The plain is primarily made up of doabs (the land between two rivers having a homogenous appearance). Five doabs of the region are – 
Name of Doab Rivers
Indus Sagar Doab Between the Indus and the Jhelum rivers
Chaj Doab Between the Jhelum and the Chenab rivers
Rachna Doab Between the Chenab and the Ravi rivers
Bari Doab Between the Ravi, Beas and Sutlej rivers
Bist Doab Between the Beas and the Sutlej rivers

Pic Credit – Wikimedia Commons

    • The eastern boundary of the Punjab Haryana plain is marked by the subsurface Delhi-Aravali ridge.
    • The average elevation of the plain is about 250 m above mean sea level.
    • The only river between the Yamuna and the Satluj is the Ghaggar which is considered to be the present-day Successor of the legendary Saraswati River.

Gangetic Plain

  • This is the largest unit of the Great Plain of India stretching from Delhi to Kolkata.
  • The Ganga along with its large number of tributaries originating in the Himalayas have brought large quantities of alluvium from the mountains.
  • The peninsular rivers such as Chambal, Betwa, Ken, Son, etc also contributed to the formation of this plain.
  • The general slope of the entire plain is sloping to the east and the southeast.
  • The region is marked by local prominences such as levees, bluffs, oxbow lakes, marshes, ravines, etc.
  • The regional division of Ganga Plain
    1. Upper Gangetic Plain
      • Extensive in Uttar Pradesh
      • It is divided into
    2. Middle Gangetic Plain
      • It is divided into
        • Mithila Plain – Between Gandak and Kosi (Sorrow of Bihar)
        • Magadh Plain – Located east of River Son
    3. Lower Gangetic Plains
      • Located along the foothills of the Shiwaliks. Plains are named Bengal Terai which is locally called Duars.
      • South of Terai are Bengal Bangar plains and they have lateritic accumulation that is locally called Barind plains
      • Western part of Gangetic delta is named Maribund delta, and locally called Rahr plains.
      • Gangetic delta further extends eastward – the active delta formed by Ganga and Brahmaputra is called the Sundarbans.

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