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The Indo-Gangetic Plain (Northern Plains)

Nearly a billion people live on one stretch of flat land. The Indo-Gangetic Plain, built entirely from river silt, is one of the most crowded landscapes on Earth.

Aerial view of the flat, fertile Indo-Gangetic Plain. Photo: Wikimedia Commons (public domain).
Schematic map of the Indo-Gangetic Plain, fed by the Indus, Ganga and Brahmaputra systems. Map: Jeroen, Wikimedia Commons, CC BY-SA 2.5.
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Indian Geography · IndGeo0027
The Indo-Gangetic Plain: Four Alluvial Belts
Bhabar
Narrow, porous gravel strip along the Shiwalik foothills. Rivers vanish underground here.
Tarai
Just south of Bhabar. Underground rivers re-emerge, feeding marshy, dense vegetation.
Older, higher alluvium set back from the river, with kankar (calcium-carbonate) nodules.
Younger, active floodplain. Floods almost yearly, laying down fresh fertile silt.
~700,000 km²
Total extent of the plain
3 river systems
Indus, Ganga, Brahmaputra
~1 billion
People living on the plain
Why so crowded
Flat land, deep fertile soil, and year-round river water make this the easiest large stretch of land in India to farm — which is exactly why it also became the most densely populated.
đź“‘ Contents

Must Know

  • The Indo-Gangetic Plain is a vast lowland built by the Indus, Ganga, and Brahmaputra river systems.
  • It lies between the Himalaya in the north and the Peninsular Plateau in the south.
  • The plain spans roughly 700,000 square kilometres across India, Pakistan, Nepal, and Bangladesh.
  • Within India, it covers Punjab, Haryana, Delhi, Uttar Pradesh, Bihar, West Bengal, and Assam.
  • The plain formed entirely from alluvium — silt, sand, and clay carried down and deposited by these rivers.

Good to Know

  • Geographers split the plain into four belts, based on the age and texture of the alluvium.
  • Bhabar is a narrow, porous, gravel-and-pebble strip running along the Shiwalik foothills. Rivers vanish underground here.
  • Tarai lies just south of Bhabar. The underground rivers re-emerge here, feeding marshy, densely vegetated land.
  • Bhangar is the older, higher alluvium, set back from the rivers’ active floodplains. It contains calcium-carbonate nodules called kankar.
  • Khadar is the younger, lower alluvium on the active floodplain. It floods almost every year, laying down fresh, fertile silt.

Test Yourself

1. Which three river systems built the Indo-Gangetic Plain through alluvial deposition?

 

Great to Know

  • The plain is home to close to a billion people, roughly one-seventh of the world’s population.
  • Average population density often exceeds 1,000 people per square kilometre — among the highest of any large region on Earth.
  • That density traces back to the plain’s own geology: flat land, deep fertile soil, and year-round river water make it exceptionally easy to farm.
  • Khadar’s annual flooding is a double-edged trait. It renews soil fertility for free, but also brings recurring flood risk to the same farmland.

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