Chapter 5 · 16 min read

Indo-Gangetic-Brahmaputra Plain

Overview

The Indo-Gangetic-Brahmaputra Plain (also called the Great Plain of India or Northern Plains) is:

  • The world's largest alluvial tract — formed by sediment deposited by the Indus, Ganga, and Brahmaputra river systems.
  • A monotonous, featureless, and very flat region — average elevation only ~200 m above sea level.
  • A youthful, geologically active region — still settling and accumulating sediment; prone to tectonic forces.
  • One of the world's most densely populated agricultural regions — supports more than half of India's population on roughly one-fourth of the land area.

Formation

  • When the Himalayas were uplifted (~50 Ma onwards), the area between the young fold mountains and the ancient Peninsular Shield became a down-warped foreland basin (also called the Himalayan foredeep).
  • Rivers eroding the Himalayas — Indus, Ganga, Brahmaputra and their tributaries — deposited enormous quantities of sediment into this basin over millions of years.
  • The result: an extremely deep alluvial fill (1,000–6,100 m thick) over the original bedrock.

Physical Dimensions

FeatureValue
Total length~3,200 km (India portion: ~2,400 km)
Average width150–300 km
Maximum width~500 km (in the west — Punjab region)
Width decreasesToward the east (Brahmaputra plain is narrower)
Average depth of alluvium1,000–2,000 m
Maximum depth of alluvium~6,100 m (deepest near the Himalayan foothills)
Average elevation~200 m above sea level
Highest pointNear Ambala (~291 m) — watershed between Indus and Ganga systems
Average gradientSaharanpur → Kolkata: 20 cm per km; Varanasi → Ganga delta: 15 cm per km

Boundaries

DirectionBoundary Feature
NorthShiwalik Hills (sub-Himalayas)
SouthPeninsular India (Deccan plateau edge)
WestSulaiman and Kirthar ranges (Pakistan-Afghanistan border)
EastPurvanchal Hills (Patkai, Naga, Lushai ranges)

Physiographic Zones (North → South)

The northern plains are divided into 4 parallel zones running roughly east–west from the Himalayan foothills southward:

1. The Bhabar

FeatureDetail
Width8–10 km
LocationNorthernmost strip — along foothills of the Shiwaliks
ExtentContinuous from the Indus to the Teesta; narrower in the east, wider in the west
FormationAmalgamation of alluvial fans where Himalayan rivers exit narrow mountain valleys onto the flat plain
Key featureHighly porous — rivers disappear underground; streams have dry courses except in the rainy season
SoilPebbles and rock debris; coarse, impermeable for fine roots
AgricultureNot suitable for farming — only large trees with deep tap roots survive

Alluvial fan: Fan-shaped sediment deposit (gravel, sand, silt) where a stream exits a narrow valley. Streams lose velocity abruptly → drop sediment → spread out like a fan.


2. The Tarai (Terai)

FeatureDetail
Width10–20 km
LocationImmediately south of the Bhabar, running parallel to it
FormationUnderground streams from the Bhabar re-emerge as they hit the impermeable surface below
CharacterIll-drained, damp, marshy
RainfallMore pronounced in the east (higher rainfall) than the west
VegetationThickly forested — supports diverse wildlife
SoilSilty; rich in nitrogen and organic matter; deficient in phosphate

Important Wildlife Areas in Tarai:

  • Jim Corbett National Park (Uttarakhand) — first national park in India (1936); home of Bengal tiger
  • Kaziranga National Park (Assam) — UNESCO WHS; famous for one-horned rhinoceros
  • Dudhwa National Park (UP)
  • Royal Chitwan National Park (Nepal border)

Agricultural use: Large tracts of Tarai (Punjab, UP, Uttarakhand) converted to farmland — major producer of sugarcane, rice, wheat.


3. Alluvial Plains

South of the Tarai — the main body of the Great Plain; divided into:

Bhangar (Old Alluvium)

FeatureDetail
PositionAbove floodplains; terrace-like high ground
AgeOlder alluvium (Pleistocene)
SoilMore clayey, generally darker in colour
Distinguishing featureContains Kankar — calcareous concretions (lime nodules) formed by calcium carbonate precipitation
FossilsAnimal fossils (rhinoceroses, hippopotamuses, elephants) — shows former tropical conditions
Sub-typesBarind plains (Bengal delta area); Bhur formations (upper Ganga-Yamuna doab)

Barind Plains: High, undulating region in the Bengal delta area (NW of upper Padma-Jamuna confluence); reddish-yellowish clay soils; cut by ravines; divided by the Atrai River.

Bhur: Elevated windblown sand accumulations in the upper Ganga–Yamuna Doab — formed during hot, dry months; less fertile.

Reh / Kollar: Saline efflorescence (white salt crust) on the surface of Bhangar soils in Haryana and western UP — caused by capillary rise of saline groundwater, worsened by excessive irrigation.

Khadar (New Alluvium)

FeatureDetail
PositionAlong riverbanks — active floodplains
AgeNewer (Holocene — ongoing deposition)
SoilSandy clays and loams; lighter, drier, more leached, less calcareous
FertilityRenewed annually by river flooding → most fertile alluvial sub-type
LandformsSandbars, meanders, ox-bow lakes, braided channels, levees

4. Delta Plains

  • Formed where rivers reach the sea — drop all remaining sediment.
  • Feature: featureless, very low gradient (2 cm per km in Sundarbans).
  • General elevation: 50–150 m above sea level (except delta areas which are near sea level).
  • World-class deltas in India: Ganga–Brahmaputra–Meghna (Sundarbans), Mahanadi, Godavari, Krishna, Cauvery.

Regional Divisions

1. Sindh Plain (primarily in Pakistan)

  • Mainly Bhangar Plains.
  • Dhors: Long, narrow depressions representing remnants of former river courses.
  • Dhand: Alkaline lakes on some Dhors.

2. Rajasthan Plain

  • Located west of the Aravallis — average elevation ~325 m.
  • Appears like an aggradational plain but contains outcrops of gneisses, schists, and granites → geological connection to the Peninsular Plateau.
  • Divided from east to west:
    • Rajasthan Bagar (semi-arid, east) → Marwar (arid) → Thar Desert (extremely arid, west)
    • Rohi: Fertile patches in the Bagar region watered by seasonal Aravalli streams.

Thar Desert (Great Indian Desert)

FeatureValue
LocationNW of Aravallis; primarily Rajasthan; also parts of Punjab, Haryana, Gujarat
Annual rainfall<150 mm
TopographyUndulating; longitudinal dunes and barchans (crescent-shaped sand dunes)
Local nameMarusthali ("land of death")
Sand dune typeShifting dunes called Dhrian (local) in western part; eastern Marusthali is rocky

Geological origin:

  • Underlain by Peninsular Plateau rocks — an extension of the ancient shield.
  • During the Mesozoic era, this region was under the sea — evidenced by:
    • Wood Fossils Park at Aakal (near Jaisalmer): 180-million-year-old petrified wood.
    • Marine deposits near Brahmsar (Jaisalmer): ancient seafloor sediments.
  • Present desert features shaped by wind and arid weathering — overrides the rock structure below.

Drainage:

  • Most rivers are ephemeral — flow briefly after rain, then disappear into sand or join inland playas.
  • Streams drain into saline lakes or playas (inland drainage — does NOT reach the sea).
  • Luni River: Only significant river — seasonal; flows south into the Rann of Kutch.
    • Area north of Luni = Thali (sandy plain).

Saline Lakes (north of Luni — inland drainage basin):

LakeLocation
Sambhar LakeNear Jaipur — largest saline lake in India
DidwanaNagaur district
KuchamanNagaur district
DeganaNagaur district
Sargol, KhatuRajasthan

[UPSC Prelims 2021] Didwana, Kuchaman, Sargol and Khatu are names of: d) saline lakes ✓ — all in Rajasthan's inland drainage zone.

Desert slope: Northern part slopes toward Sindh (Pakistan); southern part slopes toward the Rann of Kachchh.


3. Punjab Plain (Indus Plain in India)

  • Punjab = "Panch + Aab" (Persian) = "Land of Five Rivers" (Jhelum, Chenab, Ravi, Sutlej, Beas — all Indus tributaries).
  • Plain is composed of Doabs — land areas between two rivers.

The 5 Doabs of the Punjab:

DoabRivers Bounding itLocation
Bist Doab (Jalandhar Doab)Beas (west) + Sutlej (east)India's Punjab (largest Doab in Indian portion)
Bari Doab (Majha)Beas (west) + Ravi (east)Amritsar region
Rechna DoabRavi (west) + Chenab (east)Mostly Pakistan
Jech Doab (Chaj Doab)Jhelum (west) + Chenab (east)Mostly Pakistan
Sindh Sagar DoabIndus (west) + Jhelum (east)Pakistan

Other features:

  • Average elevation: ~250 m above sea level.
  • Eastern boundary: Delhi–Aravalli ridge (divides Punjab-Haryana plain from Ganga plain).
  • Northern Punjab: Shiwalik hills eroded by Chos (numerous small streams) → gullying and ravine formation.
  • South of Sutlej: Malwa Plain (Indian Punjab).
  • Haryana Tract: Region between Ghaggar and Yamuna rivers — water divide between Yamuna and Sutlej systems.
  • Ghaggar River: Only significant river between Yamuna and Sutlej; believed to be the modern remnant of the legendary Saraswati River.

4. Ganga Plain

  • Largest section of the Great Plain — extends from Delhi to Kolkata; ~3.75 lakh km².
  • Formed by: Ganga + Himalayan tributaries (Yamuna, Ramganga, Ghaghra, Gandak, Kosi) + Peninsular tributaries (Chambal, Betwa, Ken, Son).

Sub-regions of the Ganga Plain

Upper Ganga Plain (Delhi → western UP):

Sub-regionDetail
Rohilkhand PlainNorthern UP; between Himalayas and Ganga
Ganga–Yamuna DoabLargest doab in India; between Ganga and Yamuna rivers
Yamuna–Chambal BasinBadlands — extensive Chambal ravines formed by gully erosion; major soil erosion zone

Middle Ganga Plain (eastern UP + Bihar):

Sub-regionDetail
Avadh PlainCentral UP; site of ancient Kosala kingdom (Ayodhya)
Mithila PlainBihar + Nepal Terai; Gandak–Kosi–Mahananda belt
Magadh PlainSouthern Bihar; Son River valley; site of ancient Magadha empire

Lower Ganga Plain (West Bengal + Bangladesh):

  • Braided channels, ox-bow lakes, marshes, delta plains.
  • Forms the Sundarbans delta (see below).
  • Kosi River ("Sorrow of Bihar"): Famous for frequent course changes — it has shifted ~120 km westward over the last 200 years due to heavy sediment load building up the channel bed.

5. Brahmaputra Plain (Assam Valley)

FeatureDetail
Also known asAssam Valley
BoundariesEastern Himalayas (north), Patkai + Naga Hills (east), Garo–Khasi–Jaintia + Mikir Hills (south), Indo-Bangladesh border + Lower Ganga Plain (west)
FormationSediment from Brahmaputra and its tributaries
CharacterExtensive braided river system; numerous riverine islands (Chars)
TeraiCoarse alluvial fans from northern tributaries create semi-Tarai conditions

Majuli Island — Updated 2025:

FactValue
StatusWorld's largest river island (Guinness World Records confirmed)
LocationBrahmaputra River, Jorhat district, Assam
Bounded bySubansiri River (north) + Brahmaputra River (south)
Peak area (early 20th century)~1,250 km²
Area by 2014~483 km²
Area (LANDSAT 2023)~474 km² — still shrinking
Villages lost since 199135+
Cause of erosionBrahmaputra's powerful flooding + upstream embankments that concentrate erosive force; climate change amplifying monsoon intensity
Cultural significanceCentre of Vaishnava culture (Satras — Vaishnavite monasteries); recognized as first island district of India (2016)

UPSC Trap: Some older sources cite Majuli's area as 880 km² or 920 km². The most recent verified figure (2023 satellite data) is ~474 km². The island has lost over 60% of its original area.


6. Ganga–Brahmaputra Delta: Sundarbans

FeatureDetail
FormationConfluence of Ganges (Hooghly, Padma), Brahmaputra, and Meghna rivers at the Bay of Bengal
TypeWorld's largest delta (by area) and fastest-growing delta
Total area~10,277 km²
India's portion~4,260 km² (South + North 24 Parganas, West Bengal)
Bangladesh portion~6,017 km² (Khulna Division)
UNESCO WHSSundarbans National Park inscribed 1987; Sundarbans Biosphere Reserve expanded 1997
Name originFrom Sundri tree (Heritiera fomes) — dominant mangrove species
Gradient~2 cm per km — almost perfectly flat
Sea level vulnerabilityTwo-thirds of area is below 30 m above sea level
Key wildlifeRoyal Bengal Tiger (largest single tiger population); Irrawaddy dolphins; Olive Ridley turtles; Fishing cats
Forest typeWorld's largest contiguous mangrove forest
Forest characterSeaward side: estuaries, mudflats, mangrove swamps, sandbanks, islands, forelands

Note: The Indian portion is managed under Sundarbans National Park + Tiger Reserve; the Bangladesh portion (Sundarbans Reserve Forest) is the largest single mangrove forest block in the world by area.


Significance of the Indo-Gangetic-Brahmaputra Plain

DimensionSignificance
PopulationHouses more than half of India's population on ~one-fourth of the land area — most densely settled agricultural region on Earth
AgricultureFertile alluvial soils + flat terrain + slow perennial rivers + favourable climate = intense cultivation; Punjab–Haryana–western UP = granary of India (Green Revolution epicentre)
IrrigationMost irrigated region in the world; tube wells, canals, and tanks extensively used
TransportFlat terrain → dense road and rail network; connected all major cities
IndustryTextile mills (UP, Punjab), sugar mills, jute mills (WB) — proximity to raw materials and dense population
CulturalBirthplace of Indus Valley Civilization, Vedic culture, Mauryan empire, Mughal empire; Ganga is India's sacred river; pilgrimage towns (Varanasi, Haridwar, Prayagraj, Mathura)
MineralsNo metallic minerals (alluvial cover too thick); but coal near delta transition (WB), petroleum in Assam Valley and Rajasthan

UPSC Corner

Key One-Liners for Prelims

  • Indo-Gangetic-Brahmaputra Plain = world's largest alluvial tract; total length ~3,200 km
  • Alluvium depth: average 1,000–2,000 m; maximum ~6,100 m
  • Average gradient: 20 cm/km (Saharanpur → Kolkata); flattens to 15 cm/km near delta
  • Ambala (~291 m): highest point of the northern plains; watershed between Indus and Ganga systems
  • 4 physiographic zones (N→S): Bhabar → Tarai → Alluvial (Bhangar + Khadar) → Delta
  • Bhabar (8–10 km wide): porous, rivers disappear underground; not suitable for farming
  • Tarai: underground streams re-emerge; marshy; Jim Corbett (Uttarakhand), Kaziranga (Assam)
  • Bhangar = older alluvium; terrace-like; Kankar nodules; animal fossils
  • Khadar = newer alluvium; floodplains; most fertile; renewed annually
  • Reh/Kollar = saline efflorescence; excess irrigation problem in Haryana/western UP
  • Bhur = windblown sand accumulations in upper Ganga–Yamuna Doab
  • Sambhar Lake = largest saline lake in India; Rajasthan; inland drainage basin
  • Luni River: only significant river in Thar Desert; drains south into Rann of Kutch; seasonal
  • Punjab = "Land of Five Rivers" (Jhelum, Chenab, Ravi, Sutlej, Beas)
  • Doab = land between two rivers; India's largest doab = Ganga–Yamuna Doab
  • Kosi River = "Sorrow of Bihar" — shifted ~120 km west over 200 years due to heavy sediment
  • Ghaggar River = sole river between Yamuna and Sutlej; considered remnant of Saraswati
  • Majuli Island (Assam): world's largest river island (Guinness); area ~474 km² (2023); was 1,250 km²; losing area to Brahmaputra erosion
  • Chars = small riverine islands in Brahmaputra formed by extensive braiding
  • Sundarbans: ~10,277 km² total; India: ~4,260 km², Bangladesh: ~6,017 km²; UNESCO WHS 1987; gradient = 2 cm/km
  • Sundarbans = named after Sundri tree (Heritiera fomes); home of Royal Bengal Tiger
  • Thar Desert: Mesozoic sea evidence at Aakal Wood Fossils Park (180 Ma wood) + marine deposits near Brahmsar, Jaisalmer

Mains GS1 Questions

  1. "Describe the physiographic zones of the Indo-Gangetic Plain from north to south and explain the significance of each zone."
  2. "What is the Thar Desert? Discuss its physical characteristics and explain how it came to occupy a place on the Peninsular Plateau extension."
  3. "Examine the factors that make the Indo-Gangetic Plain the most densely populated region in India."
  4. "Majuli Island in Assam is facing an existential threat. Discuss the causes and implications of its shrinkage."

MCQ Trap Awareness

  • Trap: "Bhabar is suitable for agriculture" → Wrong — Bhabar is too porous and coarse; rivers disappear; only large trees with deep roots survive.
  • Trap: "Tarai is north of Bhabar" → Wrong — Tarai is south of Bhabar (water flows down and re-emerges).
  • Trap: "Bhangar is the newer/younger alluvium" → WrongBhangar = older; Khadar = newer.
  • Trap: "Bhangar soils are more fertile than Khadar" → WrongKhadar is more fertile (renewed annually by floods); Bhangar has Kankar and is older.
  • Trap: "Luni River is a perennial river" → Wrong — Luni is a seasonal river (ephemeral in drier years).
  • Trap: "Sambhar Lake is a freshwater lake" → Wrong — Sambhar is India's largest saline lake (not freshwater).
  • Trap: "Punjab means Land of Five Lakes" → Wrong — Punjab = "Land of Five Rivers" (Panch + Aab in Persian).
  • Trap: "Kosi River is called the Sorrow of Assam" → Wrong — Kosi is "Sorrow of Bihar" (its frequent course changes flood Bihar plains).
  • Trap: "Majuli is the world's largest delta island" → Wrong — Majuli is the world's largest river island (not delta); Sundarbans is the largest delta.
  • Trap: "Sundarbans is only in India" → Wrong — Sundarbans straddles India (~4,260 km²) and Bangladesh (~6,017 km²).
  • Trap: "Ghaggar is a tributary of the Ganga" → Wrong — Ghaggar is an independent river that eventually disappears in the Thar Desert; it is the water divide between Yamuna and Sutlej.
  • Trap: "Thar Desert has no geological age evidence" → Wrong — Aakal Wood Fossils Park (Jaisalmer) proves the region was forested and under the sea ~180 Ma (Mesozoic).
  • Trap: "Majuli island area is 880 km²" → Outdated — area has shrunk to ~474 km² as of 2023 satellite data.
Key Facts(24 of 80)
1 UPSC PYQ

UPSC Previously Asked

  • UPSC Trap: Some older sources cite Majuli's area as 880 km² or 920 km². The most recent verified figure (2023 satellite data) is ~474 km². The island has lost over 60% of its original area.

The world's largest alluvial tract — formed by sediment deposited by the Indus, Ganga, and Brahmaputra river systems.

A monotonous, featureless, and very flat region — average elevation only ~200 m above sea level.

A youthful, geologically active region — still settling and accumulating sediment; prone to tectonic forces.

One of the world's most densely populated agricultural regions — supports more than half of India's population on roughly one-fourth of the land area.

When the Himalayas were uplifted (~50 Ma onwards), the area between the young fold mountains and the ancient Peninsular Shield became a down-warped foreland basin (also called the Himalayan foredeep).

The result: an extremely deep alluvial fill (1,000–6,100 m thick) over the original bedrock.

Jim Corbett National Park (Uttarakhand) — first national park in India (1936); home of Bengal tiger

Kaziranga National Park (Assam) — UNESCO WHS; famous for one-horned rhinoceros

Dudhwa National Park (UP)

Royal Chitwan National Park (Nepal border)

Feature: featureless, very low gradient (2 cm per km in Sundarbans).

Dhors: Long, narrow depressions representing remnants of former river courses.

Dhand: Alkaline lakes on some Dhors.

Located west of the Aravallis — average elevation ~325 m.

Appears like an aggradational plain but contains outcrops of gneisses, schists, and granites → geological connection to the Peninsular Plateau.

Rajasthan Bagar (semi-arid, east) → Marwar (arid) → Thar Desert (extremely arid, west)

Rohi: Fertile patches in the Bagar region watered by seasonal Aravalli streams.

Underlain by Peninsular Plateau rocks — an extension of the ancient shield.

During the Mesozoic era, this region was under the sea — evidenced by:

Wood Fossils Park at Aakal (near Jaisalmer): 180-million-year-old petrified wood.

Marine deposits near Brahmsar (Jaisalmer): ancient seafloor sediments.

Present desert features shaped by wind and arid weathering — overrides the rock structure below.

Most rivers are ephemeral — flow briefly after rain, then disappear into sand or join inland playas.