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Drainage System of Rajasthan

Part of the RPSC RAS study roadmap. General Studies topic geogra-003 of General Studies.

Drainage System of Rajasthan

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Rajasthan has a complex drainage system — most rivers are seasonal (non-perennial), dependent on monsoon rainfall, and many of the smaller ones do not reach the sea. The state has three major river basins: the Yamuna (Ganga) system, the Indus system, and the Luni system (endorheic).

Key Facts for RPSC RAS:

  • The Chambal River is the most important river in Rajasthan — a tributary of the Yamuna, flowing through the deep ravines of the Dholpur and Karauli districts.
  • The Luni River is the longest river in Rajasthan (approximately 511 km) — flows from the Aravalli hills near Ajmer and terminates in the Rann of Kutch (not the sea).
  • The Ghaggar River (also called the Saraswati in its upper reaches) is a significant seasonal river that flows through northern Rajasthan.
  • Most rivers in western Rajasthan are ephemeral — flowing only during and immediately after the monsoon.
  • The Indira Gandhi Canal is not a natural river but a major man-made waterway that transforms the desert landscape.

⚡ Exam tip: The Chambal River’sravine system, the Luni River basin, and the distinction between endorheic (closed) and exorheic (open) drainage are frequently asked in RAS.


🟡 Standard — Regular Study (2d–2mo)

Standard content for students with a few days to months.

Classification of Rivers

Rajasthan’s rivers can be classified by their drainage patterns and ultimate destination:

Exorheic (Open) Drainage — Flow to the Sea

These rivers flow out of Rajasthan and eventually reach the sea:

1. Chambal River System:

  • Origin: Near Mhow (Madhya Pradesh), in the Vindhyan plateau
  • Length in Rajasthan: Approximately 400 km
  • Major tributaries: Banas, Kothari, Kalisindh, Parvati, Mej
  • Route in Rajasthan: Enters Rajasthan near Dholpur, flows through Bharatpur and Kota, joins the Yamuna near Etawah (Uttar Pradesh)
  • Significance: Longest undammed river in the Chambal-Yamuna system; home to the critically endangered Gharial (Gavialis gangeticus) and Ganges River Dolphin
  • The Chambal Ravines: The deep ravines (gorges) of the Chambal near Dholpur and Karauli are famous — they were historically difficult terrain for armies and were used by dacoits (famous dacoits like Phoolan Devi operated here)

2. Banas River:

  • Origin: Aravalli hills near Kumbhalgarh (Rajsamand district)
  • Length: Approximately 512 km
  • Route: Flows east through Bhilwara, Bundi, and Kota, joins Chambal near Tetiah in Sawai Madhopur
  • Tributaries: Bedach, Kothari, and other smaller streams
  • Significance: Major tributary of Chambal; significant for irrigation

Endorheic (Closed) Drainage — Do Not Reach the Sea

These rivers flow inland and terminate in lakes, marshes, or simply dry up:

1. Luni River (Sadhmanta):

  • Origin: Near Ajmer in the Aravalli hills (the western slopes)
  • Length: Approximately 511 km (longest river entirely within Rajasthan)
  • Route: Flows southwest through Ajmer, Pali, Jodhpur, and Barmer, eventually draining into the Rann of Kutch (in Gujarat) — but in most years it dries up before reaching the Rann
  • Major tributaries: Jawai, Sukri, Guhi, Bandi
  • Name: Called “Luni” (salty) because its water becomes increasingly saline as it flows west
  • Significance: The only major river that provides water to the Jodhpur region; lifeline of Marwar

2. Ghaggar-Hakra River:

  • Origin: Himalayas (in Himachal Pradesh), flows through Haryana and then into Rajasthan
  • Route in Rajasthan: Flows through Ganganagar and Bikaner districts, eventually dries up in the Thar Desert
  • Identification: Identified by most scholars as the Saraswati River of ancient texts — the “Naditama” (greatest river) of the Rigveda
  • Tributaries: Chautang, Tangri

3. Kantli, Koli, and Sabi Rivers:

  • Smaller rivers of the eastern plains that flow seasonally and terminate in inland depressions

Rivers of Western Rajasthan

The western desert region has virtually no perennial rivers — only khades (natural depressions) and saras (shallow lakes) that fill during monsoon:

  • Banas River in its upper reaches is seasonal in the desert
  • Guhi River (tributary of Luni) is the only significant seasonal river
  • Mendha River — a tributary of Luni near Jodhpur

🔴 Extended — Deep Study (3mo+)

Comprehensive coverage for students on a longer study timeline.

Detailed Analysis of Major River Systems

The Chambal — Detailed Profile

The Chambal is not just any river — it is the ecological and historical lifeline of eastern Rajasthan:

Hydrology:

  • Mean annual flow at Dholpur: approximately 2,400 cubic metres per second during monsoon
  • Dry season flow: drops to less than 100 cumecs
  • The river’s gradient is relatively gentle, creating wide floodplains in some areas and deep ravines in others

The Ravine System: The Chambal and its tributaries (particularly the Banas) have carved deep ravines (gullies) into the soft alluvial soil of eastern Rajasthan. This is one of the most severe soil erosion zones in India:

  • Erosion rates of up to 50 tonnes per hectare annually in some areas
  • The ravines near Dholpur and Karauli extend up to 30 km inland from the river
  • These ravines were historically inaccessible — nawabs used them as hideouts

Chambal Conservation Project: The Government of India has launched the Chambal ravine reclamation programme to prevent further soil erosion and restore agricultural land. Contour bunding, plantation, and check dams are some of the measures employed.

The Chambal Gharial Sanctuary: The National Chambal Sanctuary (established 1984) covers the Chambal river and its banks across Rajasthan, Madhya Pradesh, and Uttar Pradesh. It protects:

  • Gharial (Gavialis gangeticus) — critically endangered; approximately 1,500 remain in the wild
  • Ganges River Dolphin (Platanista gangetica)
  • Indian Skimmer (Rynchops albicollis)
  • Freshwater turtles and over 150 species of birds

The Luni River — Marwar’s Lifeline

The Luni is unique — it is the only major river in the Marwar region and has shaped the civilization of Jodhpur, Pali, and Barmer:

Salinity Problem:

  • “Luni” means “salty” — as the river flows west, it passes through increasingly saline soils
  • In the desert, water table is high and capillary action brings salts to the surface
  • The river’s lower reaches are too saline for human consumption
  • However, the upper reaches (near Ajmer and Pali) provide critical freshwater

Flooding: During heavy monsoon years, the Luni can become a violent flood river:

  • The 2010 floods of the Luni caused significant damage in Barmer and Jalore
  • The river can swell from a trickle to a 10-km-wide flood in 24 hours

The Saraswati-Ghaggar Connection

The Ghaggar River is central to understanding ancient Indian civilization:

The Saraswati of the Vedas:

  • Most Vedic scholars identify the Ghaggar-Hakra with the Saraswati River
  • The Rigveda (10,000+ verses) mentions Saraswati as the greatest of rivers — “Saraswati, the best of mothers, best of rivers”
  • The Saraswati is described as flowing from the mountains to the sea (“saptasindhava”)
  • The Saraswati dried up approximately 4,000-5,000 years ago due to climate change and river course changes

Ghaggar as Evidence of Ancient Civilisation:

  • Major Harappan sites (e.g., Rakhigarhi in Haryana) are located on the Ghaggar banks
  • The decline of the Ghaggar may have contributed to the decline of the Harappan civilization
  • Some scholars argue the Saraswati shifted its course eastward to join the Ganga system, abandoning its original course

Water Conservation — Dams and Reservoirs

Rajasthan has built significant water infrastructure to cope with its erratic rainfall:

Major Dams:

DamRiverDistrictPurpose
Mahi DamMahiBanswaraIrrigation, flood control
Jawahar SagarChambalKotaHydropower
Ranapratap SagarChambalChittorgarhIrrigation, power
Kota BarrageChambalKotaIrrigation
Bisalpur DamBanasTonkDrinking water (Jaipur)
Nakki LakeMount AbuNatural, sacred

Indira Gandhi Canal — The Lifeline of Western Rajasthan: The Indira Gandhi Canal (originally the Rajasthan Canal) is India’s largest canal project:

  • Source: Pong Dam reservoir (Beas River) in Himachal Pradesh
  • Length: 649 km ( Rajasthan portion)
  • Coverage: Intended to bring irrigation to 1.5 million hectares of the Thar Desert
  • Beneficiary districts: Bikaner, Jaisalmer, Barmer, Jodhpur, Nagaur, Churu
  • Stages: Stage I from Harike (Punjab) to Rajasthan border; Stage II into western Rajasthan

Environmental concerns:

  • Soil salinity from rising water tables
  • Changes in desert ecology
  • Potential for waterlogging if not properly managed
  • The canal has transformed desert to farmland — with mixed ecological consequences

Lakes of Rajasthan

Rajasthan has several important natural and artificial lakes:

Udaipur’s Lake Palace on Lake Pichola — one of the most famous lake systems in India:

  • Lake Pichola (built 1560s by Maharana Udai Singh II)
  • Fateh Sagar (1679, rebuilt 1889)
  • Udai Sagar (1560s)
  • These lakes are fed by Aravalli streams and serve as critical freshwater reserves for Udaipur

Other notable lakes:

  • Nakki Lake (Mount Abu) — sacred lake, allegedly created by divine nails
  • Anasagar (Ajmer) — artificial lake with the Shah Jahan-built Baradari
  • Nakki — the largest natural lake in the Udaipur region
  • Salt lakes of Sambhar and Didwana — used for salt production

Practice Questions for RPSC RAS

  1. Differentiate between endorheic and exorheic drainage systems with specific examples from Rajasthan.
  2. Explain the ecological importance of the Chambal River and the threats it faces.
  3. How has the Luni River shaped the civilization of Marwar? Discuss its salinity problem.
  4. What is the significance of the Ghaggar River in the context of the ancient Saraswati civilization?
  5. Evaluate the impact of the Indira Gandhi Canal on western Rajasthan’s ecology and economy.

Common Mistakes to Avoid

  • Confusing the Luni with the Indus — the Luni is entirely within Rajasthan and ends in the Rann of Kutch, not the Arabian Sea.
  • Thinking all rivers are perennial — most rivers in western Rajasthan are seasonal/ephemeral.
  • Missing the Ghaggar-Saraswati connection — this is a major topic in ancient history and geography.

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