Rajasthan has an arid to semi-arid climatic condition and hence its drainage system is mainly inland. It has got rivers flowing into the Arabian Sea or Bay of Bengal or at the end in salt lakes and basins. Important rivers are Chambal, Banas, Luni and Sabarmati. Patterns of drainage range between dendritic and those that are radial and annular. These systems are essential to understand how to manage the limited water sources in Rajasthan.
Key Points for RAS Mains
Context
- Rajasthan is the largest state of India which is also a rain-shadow area and hence it experiences poor rainfall as well as a poorly developed drainage system.
- This has created the geographical and climatic states of the state, which have determined the river systems and the water flow pattern in the state.
Classification of Rajasthan’s Drainage System
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Type
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Details
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Arabian Sea Drainage
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Rivers: Luni, Sabarmati, Mahi
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Bay of Bengal Drainage
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Rivers: Chambal, Banas, Banganga, Parbati
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Inland (Endorheic) Drainage
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Rivers that end in inland basins/lakes e.g., Kantli, Ghaggar, and ephemeral streams
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Major Rivers of Rajasthan

1. Bay of Bengal Drainage System (20 percent)
These rivers end up meeting the Yamuna-Ganga system and flowing into the Bay of Bengal.
- Major Rivers:
- Chambal River:
- Place of origin: Janapav Hills, MP
- Flows through Kota, Sawai Madhopur, Dholpur
- Characteristics: it is a perennial river, one of the major tributaries of Yamuna.
- Banas River:
- Source: Khamnor Hills, Rajsamand
- Meets Chambal at Rameshwar ( Kota )
- Banganga River:
- Made In: Bairath Hills (Jaipur)
- Flows through Bharatpur, joins Yamuna at Fatehabad(U.P.)
2. Arabian Sea Drainage System (10%)
The end result of these rivers is that they flow west ending up in the Arabian Sea.
- Major Rivers:
- Luni River:
- Birthplace: Naga Hills (Ajmer)
- Passes through: Pali, Barmer, Jalore
- Rann of Kutch (seasonal river)
- Sub tributaries- Jawai, Sukri, Bandi
- Sabarmati River:
- Dhebar Lake, Udaipur
- drainage basin into the Arabian Sea (via Gujarat)
- Mahi River:
- Madhya Pradesh: Place of origin
- Banswara (Rajasthan) - makes up Mahi Bajaj Sagar Dam
- drainage basin into the Arabian Sea (via Gujarat)
3. Inland (Endorheic) Drainage System ( 70%)
- These rivers dry up and end at ports of salt waters or deserts.
- Key Features:
- Dominant western Rajasthan (Thar Desert)
- Mostly Rivers are ephemeral and Flow only when it rains (During monsoons)
- Major Rivers:
- Ghaggar River:
- Place of origin: Shivalik Hill, Haryana
- Flow: by Hanumangarh & Sriganganagar
- Association with mythology:The Saraswati River
- Kantli River:
- Jhunjhunu through which it flows and drains into desert basin
- Other temporal brooks:
- Seasonal, rain-fed, evaporate in the desert or depressions
Drainage Patterns in Rajasthan
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Type of Pattern
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Characteristic
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Example
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Dendritic
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Branch-like; most common
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Chambal, Banas
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Radial
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Streams radiate from a central peak or dome
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Mount Abu Region
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Trellis
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Rectangular patterns due to folded mountains
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Parts of Aravallis
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Annular
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Circular drainage due to domes or basins
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Around Sambhar Lake
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Disappearing Streams
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Water seeps into sandy terrain
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Western Rajasthan
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Lakes and Basins as Drainage Sinks
- Sambhar Lake (Largest inland salt lake): Receives seasonal drainage from Mendha, Rupangarh rivers
- Pachpadra Lake, Didwana Lake: End points for seasonal streams
- Role: Salt production, water conservation
Significance of Drainage System in Rajasthan
- Aids in eastern Rajasthan agriculture
- The ephemeral river recharge of groundwater
- The salt-making in the salt deserts
- Environmental spirit (e.g., biodiversity) Ecological balance (e.g., wetlands)
Challenges
- The majority of the rivers are seasonal and are very much dependent on monsoon
- Shortage of water in the west districts
- Urban rivers pollution caused by domestic/agriculture sources
- Shortage inter-basin transmission of terrain
The Government Initiative
- Eastern Rajasthan Canal Project (ERCP):
- Aspires to link Chambal and tributaries with the water-stressed places
- Jal Jeevan Mission/Jal Shakti Abhiyan
- Better supply of water in rural areas
- Catch the Rain Campaign:
- Encourages rainwater harvesting and recovery of the old systems
Conclusion for RAS
Due to the climatic and topographic changes, the drainage pattern of Rajasthan comprises a combination of perennial, seasonal and vanishing rivers. It is also quite important to comprehend this rather complex drainage framework with regard to regional water management and even agriculture as well as sustainable development.
Also Read: Rivers, Lakes, and Dams of Rajasthan
Also Read: Soils of Rajasthan
FAQs related to RAS RPSC
Chambal River – a tributary of Yamuna and flows throughout the year.
Luni River – a seasonal river that ends in the Rann of Kutch.
Around 70%, mainly in western arid zones.
Sambhar Lake – the largest inland saltwater lake in India.
Ghaggar River – flows through Hanumangarh and Sriganganagar.
Bay of Bengal system via Chambal → Yamuna → Ganga.
Eastern Rajasthan Canal Project (ERCP).
Radial pattern – streams radiate from a central high point.
Recharge groundwater, support agriculture and biodiversity during monsoons.