This is a list of rivers wholly or partly in Pakistan, organised geographically by river basin, from west to east. Tributaries are listed from the mouth to the source. The longest and the largest river in Pakistan is the Indus River. Around two-thirds of water supplied for irrigation and in homes come from the Indus and its associated rivers. [1]
Some of these rivers flow only during the rainy season, so for part of the year the water may or may not reach the sea.
Tributary river of River Indus; flows from Tangir Valley District Diamer down to the river Indus with Karakuram Highway.
The Indus is a transboundary river of Asia and a trans-Himalayan river of South and Central Asia. The 3,120 km (1,940 mi) river rises in mountain springs northeast of Mount Kailash in Western Tibet, flows northwest through the disputed region of Kashmir, bends sharply to the left after the Nanga Parbat massif, and flows south-by-southwest through Pakistan, before emptying into the Arabian Sea near the port city of Karachi.
The Thar Desert, also known as the Great Indian Desert, is an arid region in the north-western part of the Indian subcontinent that covers an area of 200,000 km2 (77,000 sq mi) in India and Pakistan. It is the world's 18th-largest desert, and the world's 9th-largest hot subtropical desert.
The Sarasvati River is a deified mythological river first mentioned in the Rigveda and later in Vedic and post-Vedic texts. It played an important role in the Vedic religion, appearing in all but the fourth book of the Rigveda.
The Satluj River is the longest of the five rivers that flow through the historic crossroads region of Punjab in northern India and Pakistan. The Sutlej River is also known as Satadru. It is the easternmost tributary of the Indus River. The Bhakra Dam is built around the river Sutlej to provide irrigation and other facilities to the states of Punjab, Rajasthan and Haryana.
The Chautang is a seasonal river, originating in the Sivalik Hills, in the Indian state of Haryana. The Chautang River is a tributary of the Sarsuti river which in turn is a tributary of the Ghaggar river.
The Ghaggar-Hakra River is an intermittent river in India and Pakistan that flows only during the monsoon season. The river is known as Ghaggar before the Ottu barrage at 29.4875°N 74.8925°E, and as Hakra downstream of the barrage in the Thar Desert. In pre-Harappan times the Ghaggar was a tributary of the Sutlej. It is still connected to this paleochannel of the Sutlej, and possibly the Yamuna, which ended in the Nara River, presently a delta channel of the Indus River joining the sea via Sir Creek.
The Tons is the largest tributary of the Yamuna. It flows through Garhwal region in Uttarakhand, touching Himachal Pradesh. The Tons thrust is named after this river.
The Kūnaṛ River, also known as the Chitral River, Mastuj River and Kama River, is a 480 kilometres (300 mi) long river located in northern Pakistan and eastern Afghanistan. It originates just south of the Broghil Pass, in the Upper Chitral District of Khyber Pakhtunkhwa province in Pakistan. It later merges with Kabul river in the Nangahar Province of Afghanistan. The river system is fed by melting glaciers and snow of the Hindu Kush mountains. The Kunar River is a tributary of the Kabul river, which is in turn a tributary of the Indus River.
The Rigveda refers to a number of rivers located in the northwestern Indian subcontinent, from Gandhara to Kurukshetra. They are located in present-day India, Afghanistan and Pakistan.
The Rupal River is an east–west glacial stream rising from the meltwater of the Rupal Glacier in Gilgit-Baltistan region of northern Pakistan. The stream flows through the Rupal Valley, south of Nanga Parbat, before turning northeast to the village of Tarashing. The Rupal drains into the Astore River, which eventually reaches the Indus near Jaglot.
The Nara Canal is a deepened delta channel of the Indus River in Sindh province, Pakistan. It was built as an excavated channel stemming off the left bank of the Indus River to join the course of the old Nara River, a tributary c.q. paleochannel of the Indus which received water from the Ghaggar-Hakra until the Hakra dried-up, early 2nd millennium BCE.
The Sahibi river, also called the Sabi River, is an ephemeral, rain-fed river flowing through Rajasthan, Haryana and Delhi states in India. It originates in the eastern slopes of the Saiwar Protected Forest (PF) hills in Sikar District, enters Jaipur district near the foot of these hills, and after initially flowing southeast and east turns northeastwards near Shahpura and continues further till it exits Rajasthan to enter Haryana and further drains into Yamuna in Delhi, where its channeled course is also called the Najafgarh drain, which also serves as Najafgarh drain bird sanctuary. It flows for 300 km of which 157 km is in Rajasthan 100 km is in Haryana and 40 km in Delhi.
The Sarsuti river, originating in Sivalik Hills and flowing through the palaeochannel of Yamuna, is a tributary of Ghaggar river in of Haryana state of India. Its course is dotted with archaeological and religious sites dating back to post-Harrapan Mahabharata sites from Vedic period, such as Kapal Mochan, Kurukshetra, Thanesar, Brahma Sarovar, Jyotisar, Bhor Saidan and Pehowa.
The Kaushalya river, a tributary of Ghaggar river, is a river in Panchkula district of Haryana state of India.
The Tangri River, also called the Dangri River, which originates in the Shivalik Hills, is a tributary of the Ghaggar River in the Haryana state of India.
The Markanda is a river in the Indian states of Himachal Pradesh and Haryana. It is a tributary of the Ghaggar river, flowing through Sirmaur District, Ambala district and Shahabad Markanda, a town in Kurukshetra district. The Markanda river's ancient name was Aruna.
The Somb river, also spelled Som river is a tributary of Yamuna in Haryana state of India.
The Indori river, is a rain-fed river originates from Aravalli Range from Sikar district and flows through Alwar district of Rajasthan to Rewari district of Haryana and it is the longest tributary of Sahibi River which stretches to 50 km. In Delhi, it is called the Najafgarh drain or Najafgarh Nallah.
The Krishnavati river, also called Kasaunti, is a rain-fed river originates from Aravalli Range near Dariba copper mines in Rajsamand district of Rajasthan, and flows through Patan in Dausa district and Mothooka in Alwar district and then disappears in Mahendragarh district in Haryana where it used to be a tributary of Sahibi River, which in turn still is a tributary of Yamuna. Several Ochre Coloured Pottery culture sites have been found along the banks of Krishnavati, Sahibi river, Dohan river and Sota River. The drainage pattern for all these rivers is dendritic.
The Dohan river, is a rain-fed river that originates at Mandholi village near Neem Ka Thana in Sikar district of Rajasthan and then disappears in Mahendragarh district in Haryana where it used to be a tributary of Sahibi River, which in turn is a still flowing tributary of Yamuna. Its canalised portion in one of its paleochannel in Haryana is called the "Outfall Drain No 8".
It may be noted that the Nara is still called the Sarasvati by rural Sindhis and its dried up delta in Kutch is still regarded as that of Sarasvati by the locals.
