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The Luni is the largest river in the Thar Desert in Northwest India. [1] It originates in the Pushkar valley of the Aravalli Range , near Ajmer , passes through the southeastern portion of the Thar Desert, and ends in the marshy lands of Rann of Kutch in Gujarat , after travelling a distance of 495 km (308 mi).
The river flows for 48 kilometres (30 mi) before joining the Luni River in the Pali district of Rajasthan. Its drainage basin covers an area of 2,200 square kilometres (850 sq mi); the depth of the river is 5 metres (16 ft). The water quality of the Raipur Luni River is eutrophic, meaning that it is nutrient-rich.
Water Catchment Areas in Rajasthan River System Catchment Area (in square km) Banas: 46,570 Luni River: ... Luni River Sequence: 69,302: 20.25% Banas River Sequence ...
The Luni River is the only river in the desert. [16] Rainfall is 100 to 500 mm (4 to 20 in) per year, almost all of it between June and September. [3] Saltwater lakes within the Thar Desert include the Sambhar, Kuchaman, Didwana, Pachpadra, and Phalodi in Rajasthan and Kharaghoda in Gujarat. These lakes receive and collect rainwater during ...
Rajasthan (/ r ɑː dʒ ə ˈ s t ɑː n / ... (5,650 ft) in height, to Khetri in the northeast. ... The Luni River and its tributaries are the major river system of ...
Flowing in a north-east to south-west direction, it gathers water from multiple smaller streams along its path, ultimately converging with the Luni River near Khejalda Khurd in Jodhpur district. [2] This river is a tributary of Luni river. The Jojari basin is located between latitudes 26 07 and 26 43 and longitudes 73 08 and 74 00. [3] [4]
The Aravalli Range (also spelled Aravali) is a mountain range in Northern-Western India, running approximately 670 km (420 mi) in a south-west direction, starting near Delhi, passing through southern Haryana, [1] Rajasthan, and ending in Ahmedabad Gujarat.
The Luni River is the principal feature of the Marwar plains. It originates from the Pushkar valley of Ajmer district, and the main river flows through Marwar in a south-westerly direction until it finally disappears into the seasonal wetland of the Rann of Kutch in Gujarat. It is fed by tributaries that flow from the Aravallis.