Chenab River
The Chenab River is formed by the confluence of the Chandra and Bhaga rivers at Tandi located in the upper Himalayas, in the Lahul and Spiti District of Himachal Pradesh, India. In its upper reaches it is also known as the Chandrabhaga. It flows through the Jammu region of Jammu and Kashmir into the plains of the Punjab, forming the boundary between the Rechna and Jech interfluves (Doabs in Persian). It is joined by the Jhelum River at Trimmu, and then by the Ravi River. It then merges with the Sutlej River near Uch Sharif to form the Panjnad ('Five Rivers'), which joins the Indus at Mithankot. The total length of the Chenab is approximately 960 kilometres. The waters of the Chenab are allocated to Pakistan under the terms of the Indus Waters Treaty.
The river was known to Indians in Vedic period as Ashkini or Iskmati and as Acesines to the Ancient Greeks. In 325 BC, Alexander the Great allegedly founded the town of Alexandria on the Indus (present day Uch Sharif or Mithankot or Chacharan) at the confluence of the Indus and the combined stream of Punjab rivers (currently known as the Panjnad River).
The Chenab has the same place in the consciousness of the people of the Punjab, as, say the Rhine holds for the Germans, or the Danube for the Austrians and the Hungarians. It is the iconic river around which Punjabi consciousness revolves, and plays a prominent part in the tale of Heer Ranjha, the Punjabi national epic.
Dasht River
Dasht River is located in Gwadar District, Balochistan, Pakistan. Mirani Dam is being built on Dasht river to provide drinking water to Gwadar city.
Dashtiari River
Dashtiari River is located in Gwadar District, Balochistan, Pakistan.
Gambila River
Gambila River river, also called the Tochi River, is located in Bannu District, North-West Frontier Province, Pakistan.
It's source are the hills six miles south of the Sufed Koh, the source of the Kurram River, which it runs parallel too and finally joins.
The Gambila is an important river for the inhabitants of the Dawar valley, as it serves to irragate a large area of land that it runs through. Particularly that belonging to the Bakkakhel Wazirs, and Miri and Barakzai Bannuchis.
Ghaggar-Hakra River
The Ghaggar-Hakra River is the (rainy) seasonal river in India and the Hakra River riverbed in Pakistan. It is often identified with the Vedic Sarasvati River, but it is disputed if at all Rigvedic references to the Sarasvati River refer to this river. It is a dried out river which flow during rainy season only and used to flush out flood waters of Punjab.
Estimated period at which the river dried up range, very roughly, from 2500 to 2000 BC, with a further margin of error at either end of the date-range. This may be precise in geological terms, but for the Indus Valley Civilization (2800 to 1800 BC) it makes all the difference whether the river dried up in 2500 (its early phase) or 2000 (its late phase). Similarly, for the Gandhara grave culture, often identified with the early influx of Indo-Aryans from ca. 1600 BC, it makes a great difference whether the river dried up a millennium earlier, or only a few generations ago, so that by contact with remnants of the IVC like the Cemetery H culture, legendary knowledge of the event may have been acquired.
The identification with the Sarasvati River is based the descriptions in Vedic texts (e.g. in the enumeration of the rivers in Rigveda 10.75.05, the order is Ganga, Yamuna, Sarasvati, Sutlej), and other geological and paleobotanical findings. This however, is disputed. The Victorian era scholar C.F. Oldham was the first to suggest that geological events had redirected the river, and to connect it to the lost Saraswati: "[it] was formerly the Sarasvati; that name is still known amongst the people, and the famous fortress of Sarsuti or Sarasvati was built upon its banks, nearly 100 miles below the present junction with the Ghaggar." (Oldham 1893: 51-52)
Ghaggar River
The Ghaggar is a seasonal river in India, flowing when water is available from monsoon rains. It originates in the Shivalik Hills of Himachal Pradesh and flows through Punjab and Haryana to Rajasthan; just southwest of Sirsa in Haryana and by the side of Tibi in Rajasthan, this seasonal river feeds two irrigation canals that extend into Rajasthan.
The present-day Sarasvati River originates in a submontane region (Ambala district) and joins the Ghaggar near Shatrana in PEPSU. Near Sadulgarh (Hanumangarh) the Naiwala channel, a dried out channel of the Sutlej, joins the Ghaggar. Near Suratgarh the Ghaggar is then joined by the dried up Drishadvati river.
The wide river bed of the Ghaggar river suggest that the river once flowed full of water, and that it formerly continued through the entire region, in the presently dry channel of the Hakra River, possibly emptying into the Rann of Kutch. It supposedly dried up due to the capture of its tributaries by the Indus and Yamuna rivers, and the loss of rainfall in much of its catchment area due to deforestation and overgrazing. This is supposed to have happened at the latest in 1900 BCE, but perhaps much earlier.
Puri and Verma (1998) have argued that the present-day Tons River was the ancient upper-part of the Sarasvati River, which would then had been fed with Himalayan glaciers. The terrain of this river contains pebbles of quartzite and metamorphic rocks, while the lower terraces in these valleys do not contain such rocks.
In India there are also various small or middle-sized rivers called Sarasvati or Saraswati. One of them flows from the west end of the Aravalli Range into the east end of the Rann of Kutch.
Hakra River
The Hakra is the dried-out channel of a river in Pakistan that until about 2000 BC - 1500 BC was the continuation of the Ghaggar River in India.
Many settlements of the Indus Valley Civilisation have been found along the Ghaggar and Hakra rivers.
Indus Valley Civilization
The river was also of great importance to the Indus Valley Civilization. Archaeologists have suggested that the drying up of this river may have been one of the causes for the decline of the Indus Valley Civilization.
Along the course of the Ghaggar-Hakra river are many archaeological sites of the Indus Valley Civilization; but not further south than the middle of Bahawalpur district. It could be that the permanent Sarasvati ended there, and its water only reached the sea in very wet rainy seasons. It may also have been affected by much of its water being taken for irrigation.
Over 600 sites of the Indus civilization have been discovered on the Hakra-Ghaggar river and its tributaries. In contrast to this, only 90 to 96 Indus Valley sites have been discovered on the Indus and its tributaries (about 36 sites on the Indus river itself.) V.N. Misra states that over 530 Harappan sites (of the more than 800 known sites, not including Degenerate Harappan or OCP) are located on the Hakra-Ghaggar. The other sites are mainly in Kutch-Saurashtra (nearly 200 sites), Yamuna Valley (nearly 70 Late Harappan sites) and in the Indus Valley/ Baluchistan (less than 100 sites).
Early Harappan sites are mostly situated on the middle Ghaggar-Hakra river bed, and some in the Indus Valley. Most of the Mature Harappan sites are located in the middle Ghaggar-Hakra river valley, and some on the Indus and in the Kutch-Saurashtra. However in the late Harappan period the number of late Harappan sites in the middle Hakra channel and in the Indus valley diminishes, while it expands in the upper Ghaggar-Sutlej channels and in Saurashtra. The abandonement of many sites on the Hakra-Ghaggar between the Harappan and the Late Harappan phase was probably due to the drying up of the Hakra-Ghaggar river.
Because most of the Indus Valley sites are actually located on the Hakra-Ghaggar river and its tributaries and not on the Indus river, some archaeologists have proposed to use the term "Indus Sarasvati Civilization" to refer to the Harappan culture.
In a survey conducted by M.R. Mughal between 1974 and 1977, over 400 sites were mapped along 300 miles of the Hakra river. The majority of these sites were dated to the fourth or third millennium BCE.
Painted Grey Ware sites (ca. 1000 BCE) have been found on the bed and not on the banks of the Ghaggar-Hakra river.
The Ghaggar-Hakra and its ancient tributaries
Satellite photography has shown that the Ghaggar-Hakra was indeed a large river that dried up probably between ca. 2500 to 2000 B.C. The dried out Hakra river bed is between three and ten kilometers wide. Recent research indicates that the Sutlej and possibly also the Yamuna once flowed into the Saraswati river bed. The Sutlej and Yamuna Rivers have changed their courses over the time.
Paleobotanical information also documents the aridity that developed after the drying up of the river. (Gadgil and Thapar 1990 and references therein). The disappearance of the river may have been caused by earthquakes which may have led to the redirection of its tributaries. It has also been suggested that the loss of rainfall in much of its catchment area due to deforestation and overgrazing in what is now Pakistan may have also contributed to the drying up of the river.
The Ghaggar-Hakra and the Sutlej
There are no Harappan sites on the Sutlej in its present lower course, only in its upper course near the Siwaliks, and along the dried up channel of the ancient Sutlej, which indicates the Sutlej did flow into the Sarasvati at that period of time.
It has been shown by satellite imagery that at Ropar the Sutlej river suddenly flows away from the Ghaggar in a sharp turn. The beforehand narrow Ghaggar river bed itself is becoming suddenly wider at the conjunction where the Sutlej should have met the Ghaggar river. And there is a major paleochannel between the point where the Sutlej takes a sharp turn and where the Ghaggar river bed widens.
In later texts like the Mahabharata, the Rigvedic Sutudri ("swiftly flowing") is called Shatudri (Shatadru/Shatadhara), which means a river with 100 flows. The Sutlej (and the Beas and Ravi) have frequently changed their courses. The Sutlej has also probably sometimes flown into the Beas, and the combined stream sometimes in the Ghaggar River. The confluence of the Ghaggar and the Sutlej was downstream from the Kurukshetra region, where most Harappan sites are located.
The Ghaggar-Hakra and the Yamuna
There are also no Harappan sites on the present Yamuna river. There are however Painted Gray Ware (1000 - 600 BC) sites on the Yamuna channel, showing that the river must have flown in the present channel during this period. The distribution of the Painted Gray Ware sites in the Ghaggar river valley indicates that during this period the Ghaggar river was already partly dried up.
Scholars like Raikes (1968) and Suraj Bhan (1972, 1973, 1975, 1977) have shown that based on archaeological, geomorphic and sedimentological research the Yamuna may have flown into the Saraswati during Harappan times. There are several often dried out river beds (paleochannels) between the Sutlej and the Yamuna, some of them two to ten kilometres wide. They are not always visible on the ground because of excessive silting and encroachment by sand of the dried out river channels. The Yamuna may have flown into the Sarasvati river through the Chautang or the Drishadvati channel, since many Harappan sites have been discovered on these dried out river beds.
Gilgit River
Gilgit River is a tributary of the Indus River, and flows past the town of Gilgit. It is located in the Northern Areas of Kashmir, Pakistan.
Gomal River
Gomal River is a river in Afghanistan and Pakistan, with its headwaters in the south-east of Ghazni.
The headwater springs of the Gomal's main leg come together close to the fort of Babakarkol in Katawaz, a district inhabited primarily by Kharoti and Suleiman Khel Pashtuns.
The Gomal's chief tributary is the Zhob River. Within Pakistan, Gomal river surrounds South Waziristan agency, forms the boundary between the North-West Frontier Province and Balochistan. The river passes then through the Damaan plain in Kulachi Tehsil and later on through Dera Ismail Khan Tehsil and then finally falls in river Indus.
Hub River
Hub River is located in Lasbela, Balochistan, Pakistan. It forms the provincial boundary between Sindh and Balochistan, west of Karachi. Hub Dam is a large water storage reservoir constructed in 1981 on the Hub River in the arid plains north of Karachi. The reservoir supplies water for irrigation in the Lasbella district of Balochistan and drinking water for the city of Karachi. It is an important staging and wintering area for an appreciable number of waterbirds and contains a variety of fish species which increase in abundance during periods of high water. The Mahseer (Tor putitora), an indigenous riverine fish found in the Hub River, grows up to 2m in length and provides for excellent angling.It is in pakistan.
Hungol River
Hungol River or Hingol River is located in Makran, Balochistan, Pakistan.
The Hungol valley has fantastic scenery of towering cliffs, pinnacles and buttresses, the river winding between. Some 350 miles in length, the Hungol is Balochistan's longest river. Unlike most other streams in Balochistan which only flow during rare rains, the Hungol always has flowing water in it. The water is crystal–clear, reflecting the incredible blue of the sky. It makes for picture–postcard scenery. Hungol river and valley are located in Hungol National Park.
Hunza River
Hunza River is the principal river of Hunza, in the Northern Areas of Pakistan. It is formed by the confluence of the Kilik and Khunjerab nalas (gorges) which are fed by glaciers. It is joined by the Gilgit River and the Naltar River before it flows into the Indus River.
The river cuts through the Karakoram range, flowing from north to south. The Karakoram Highway crosses the Hunza River near Hunza and Nagar valleys.
Indus River
Indus is the longest and most important river in Pakistan and one of the most important rivers on the Indian subcontinent. Originating in the Tibetan plateau in the vicinity of Lake Mansarovar, the river runs a course through in Jammu and Kashmir and Northern Areas, flowing through the North in a southernly direction along the entire length of country, to merge into the Arabian Sea near Pakistan's port city Karachi. The total length of the river is 3200 km (1988 miles). The river has a total drainage area exceeding 450,000 square miles. The river's estimated annual flow stands at around 207 cubic kilometres. Beginning at the heights of the world with glaciers, the river feeds the ecosystem of temperate forests, plains and arid countryside. Together with the rivers Chenab, Ravi, Sutlej, Jhelum, Beas and the extinct Sarasvati River, the Indus forms the Sapta Sindhu ("Seven Rivers") delta in the Sindh province of Pakistan. It has 20 major tributaries.
The Indus provides the key water resources for the economy of Pakistan - especially the breadbasket of Punjab province, which accounts for most of the nation's agricultural production, and Sindh. It also supports many heavy industries and provides the main supply of potable water in Pakistan.
The ultimate source of the Indus is in Tibet; it begins at the confluence of the Sengge and Gar rivers that drain the Nganglong Kangri and Gangdise Shan mountain ranges. The Indus then flows northwest through Ladakh-Baltistan into Gilgit, just south of the Karakoram range. The Shyok, Shigar and Gilgit streams carry glacieral waters into the main river. It gradually bends to the south, coming out of the hills between Peshawar and Rawalpindi. The Indus passes gigantic gorges (15,000-17,000 feet) near the Nanga Parbat massif It swiftly flows across Hazara, and is dammed at the Tarbela Reservoir. The Kabul River joins it near Attock. The remainder of its route to the sea is in plains of the Punjab and Sind, and the river becomes slow-flowing and highly braided. It is joined by Panjnad River at Mithankot. Beyond this confluence, the river, at one time, was named as Satnad River (sat = seven, nadi = river) as the river was now carrying the waters of Kabul River, Indus River and the five Punjab rivers. Passing by Jamshoro, it ends in a large delta to the east of Thatta.
The Indus is one of the few rivers in the world that exhibit a tidal bore. The Indus system is largely fed by the snows and glaciers of the Karakoram, Hindu Kush and Himalayan ranges of Tibet, Kashmir and Northern Areas of Pakistan. The flow of the river is also determined by the seasons - it diminishes greatly in the winter, while flooding its banks in the monsoon months from July to September. There is also evidence of a steady shift in the course of the river since prehistoric times - it deviated westwards from flowing into the Rann of Kutch. It is the Official and National River of Pakistan in Urdu as Qaumi Daryaa and Sindhi it is called Daryaa Badshah ,The King River.
History
Paleolithic sites have been discovered in Pothohar, with the stone tools of the Soan Culture. In ancient Gandhara, evidence of cave dwellers dated 15,000 years ago has been discovered at Mardan.
The major cities of the Indus Valley Civilization (IVC), such as Harappa and Mohenjo Daro, date back to around 3300 BC, and represent some of the largest human habitations of the ancient world. The IVC was extended from Balochistan to Gujarat, with an upward reach to the darcon from east of River Jhelum to Rupar on the upper Sutlej. The coast settlements extended from Sutkagan Dor at Iranian border to Lothal in Gujarat. There is an Indus site on the Oxus river at Shortughai in northern Afghanistan (Kenoyer 1998:96), and the Indus site Alamgirpur at the Hindon river is located only 28 km from Delhi. To date, over 1,052 cities and settlements have been found, mainly in the general region of the Ghaggar-Hakra River and its tributaries. Among the settlements were the major urban centers of Harappa and Mohenjo-daro, as well as Lothal, Dholavira, Ganeriwala, and Rakhigarhi. Only 90 to 96 of the over 800 known Indus Valley sites have been discovered on the Indus and its tributaries. The Sutlej, now a tributary of the Indus, in Harappan times flowed into the Ghaggar-Hakra River, in the watershed of which were more Harappan sites than along the Indus.
Some scholars believe that settlements of Gandhara grave culture of the early Indo-Aryans flourished in Gandhara from 1700 to 600 BCE, when Mohenjo Daro and Harappa had already been abandoned. However many modern researchers believe that the IVC was indeed an Aryan civilization. Researchers such as professor Egbert Richter Ushanas concerning the IVC seals has said, "All the seals are based on Vedas -- Rig Veda and Atharva Veda." The name Indus is a Latinization of Hindu, in turn the Iranian variant of Sindhu, the name of the Indus in the Rigveda. Sanskrit sindhu generically means "river, stream", probably from a root sidh "to go, move"; sindhu is attested 176 times in the Rigveda, 95 times in the plural, more often used in the generic meaning. Already in the Rigveda, notably in the later hymns, the meaning of the word is narrowed to refer to the Indus river in particular, for example in the list of rivers of the Nadistuti sukta. This resulted in the anomaly of a river with masculine gender: all other Rigvedic rivers are female, not just grammatically, being imagined as goddesses and compared to cows and mares yielding milk and butter.
The Indus has formed a natural boundary between the Indian hinterland and its frontier with Afghanistan and Iran. It has been crossed by the armies of Alexander the Great - Greek forces retreated along the southern course of the river at the end of the Indian campaign. The Indus plains have also been under the domination of the Persian empire and the Kushan empire. The Muslim armies of Muhammad bin Qasim, Mahmud of Ghazni and Babur also crossed the river to strike into the inner regions of Gujarat, Punjab and Rajputana.
The word "India" is a reference to the Indus River.
Geology
The Indus River feeds the Indus submarine fan located in the Arabian Sea, which is the second largest sediment body on the Earth at around 5 million cubic kilometers of material eroded from the mountains. Studies of the sediment in the modern river indicate that the Karakoram Mountains in northern Pakistan are the single most important source of material, with the Himalaya provide the next largest contibution, mostly via the large rivers of the Punjab (i.e., the Ravi, Jhellum, Chenab and the Sutlej). Analysis of sediments from the Arabian Sea by marine geologists Peter Clift and Jerzy Blusztajn has demonstrated that prior to five million years ago the Indus was not connected to these Punjab Rivers which instead flowed east into the Ganges and were captured after that time. Earlier work, also by Peter Clift, showed that sand and silt from western Tibet was reaching the Arabian Sea by 45 million years ago, implying the existence of an ancient Indus River by that time. The delta of this proto-Indus river has subsequently been found in the Katawaz Basin, on the Afghan-Pakistan border. Most recently the Indus was paralleled by the ancient Saraswati River, which the Rigveda suggests flowed from the Himalaya between the Sutlej and the Yamuna Rivers, close to modern day Chandigarh. The Saraswati river was totally dried by 1900 BC as confirmed by archeological hydrological radio carbon datings.
Climate
The Indus delta is one of the driest in the Indian subcontinent, lying just to the west of the Thar Desert of Rajasthan - and rainfall is extraordinarily erratic owing to the passage of cyclones from the Arabian Sea. The Punjab plains, however, receive considerable rainfall from the summer monsoon: at Abbottabad the average annual rainfall is around 1,200mm (47 inches) and at Murree around 1,700mm (67 inches) with as much as 730mm (28 inches) in July and August alone. The upper basin of the Indus receives 4-8 inches of rainfall (higher in the west) in the winter months owing to northwestern winds. Higher elevations in Kashmir and the Northern Areas receives a large amount of precipitation in the form of snow, but the lower valleys are extremely dry and quite warm in the summer. Annual temperatures fall below freezing in the northern mountainous regions in the winter, while exceeding 100 degrees Fahrenheit in the plains of Punjab and Sindh in the summer. Jacobabad, which is one of the hottest spots in the world, lies to the west of the river in Sindh.
Wildlife
Accounts of the Indus valley from the times of Alexander's campaign indicate a healthy forest cover in the region, which has now considerably receded. The Mughal Emperor Babar writes of encountering rhinoceroses along its bank in his memoirs (the BaberNameh). Extensive deforestation and human interference in the ecology of the Shivalik Hills has led to a marked deterioration in vegetation and growing conditions. The Indus valley regions are arid with poor vegetation. Agriculture is sustained largely due to irrigation works.
The Blind Indus River Dolphin (Platanista gangetica minor) is a sub-species of Dolphins found only in the Indus River. It formerly also occurred in the tributaries of the Indus river. Palla fish (Hilsa ilisha) of the river is a delicacy for people living along the river. The population of fishes in the river is moderate, with Sukkur, Thatta and Kotri being the major fishing centres - all in the lower Sindh course. But damming and irrigation has made fish farming an important economic activity. Located southeast of Karachi, the large delta has been recognised by conservationists as one of the world's most important ecological regions. Here the river distributes into many marshes, streams and creeks and meets the sea at shallow levels. Here marine fishes are found in abundance, including pomfret and prawns.
Economy
The Indus is the most important supplier of water resources to the Punjab and Sindh plains - it forms the backbone of agriculture and food production in Pakistan. The river is especially critical as rainfall is meagre in the lower Indus valley. Irrigation canals were first built by the peoples of the Indus valley civilization, and later by the engineers of the Kushan Empire and the Mughal Empire. Modern irrigation was introduced by the British East India Company in 1850 - the construction of modern canals accompanied with the restoration of old canals. The British supervised the construction of one of the most complex irrigation networks in the world. The Guddu Barrage is 4,450 feet long - irrigating Sukkur, Jacobabad, Larkana and Kalat. The Sukkur Barrage serves over five million acres (20,000 km²).
After partition, the Pakistan Water and Power Development Authority undertook the construction of the Chashma-Jhelum link canal - linking the waters of the Indus and Jhelum rivers - extending water supplies to the regions of Bahawalpur and Multan. Pakistan also constructed the Tarbela Dam near Rawalpindi - standing 9,000 feet long and 470 feet high, with a 50 mile-long reservoir. The Kotri Barrage near Hyderabad is 3,000 feet long and provides additional supplies for Karachi. The Taunsa Barrage near Dera Ghazi Khan produces 100,000 kilowatts of electricity. The extensive linking of tributaries with the Indus has helped spread water resources to the valley of Peshawar, the Northwest Frontier Province. The extensive irrigation and dam projects provide the basis for Pakistan's large production of crops such as cotton, sugarcane and wheat. The dams also generate electricity for heavy industries and urban centres.
People
The inhabitants of the regions through whom the Indus river passes and forms a major natural feature and resource are diverse in ethnicity, religion, national and linguistic backgrounds. On the northern course of the river in Kashmir live the Buddhist people of Ladakh, of Tibetan stock, with Kashmiris who practise both Islam and Hinduism. As it descends into Northern Areas of Pakistan, the Indus river forms a distinctive boundary of ethnicity and cultures - upon the western banks the population is largely Pashtun, Balochi, and of other Afghan stock, with close cultural, economic and ethnic ties to Iran and Afghanistan. The eastern banks are largely populated with peoples of Punjabi stock, with smaller populations of Sindhis and people from regions in modern India. In northern Punjab and the NWFP, Pathan peoples and ethnic Pashtun tribes live alongside Punjabi peoples. In the southern portion of the Punjab province, the Serakai peoples speak a distinctive tongue and practise distinctive traditions. In the province of Sindh, peoples of Sindhi, Gujarati, Punjabi and Urdu-speaking Mohajir backgrounds form the local populations. Upon the western banks of the river live the Balochi and Pashtun peoples of Balochistan.
Modern issues
A flooded Indus river inundates the Srinagar-Kargil-Leh highway.
Due to its location and vast water resources, Indus is a strategically vital resource for Pakistan's economy and society.
Indus Waters treaty
After the partition of India in 1947, the use of the waters of the Indus and its five eastern tributaries became a major dispute between India and Pakistan. The irrigation canals of the Sutlej valley and the Bari Doab were split - with the canals lying primarily in Pakistan and the headwork dams in India - disrupting supply in some parts of Pakistan. The concern over India building large dams over various Punjab rivers that could undercut the supply flowing to Pakistan, as well as the possibility that India could divert rivers in the time of war, caused political consternation in Pakistan. Holding diplomatic talks brokered by the World Bank, India and Pakistan signed the Indus Waters Treaty in 1960. The treaty gave India the control of the three easternmost rivers of the Punjab, Sutlej, Beas and the Ravi, while Pakistan gained control of the three western rivers, Jhelum, Chenab and the Indus. India retained the right to use of the western rivers for non irrigation projects. (See discussion regarding a recent dispute about a hydroelectric project on the Chenab (not Indus) known as the Baghlighar project).
Pilgrimage
Hindu pilgrimage to holy sites alongside the river has been a source of conflict between the nations. Pakistan does generally allow Indian citizens to visit the country for religious purposes, However, owing to the volatile nature of bilateral relations, most pilgrimage and religious ceremonies are performed by Hindus in Kashmir.
Conservation
There are concerns that extensive deforestation, industrial pollution and global warming are affecting the vegetation and wildlife of the Indus delta, while affecting agricultural production as well. There are also concerns that the Indus river may be shifting its course westwards - although the progression spans centuries. On numerous occasions, Water-clogging owing to poor maintenance of canals has affected agricultural production and vegetation. In addition, extreme heat has caused water to evaporate leaving salt deposits that render lands useless for cultivation.
Jhelum River
Jehlum River or Jhelum River is the largest and most western of the five rivers of Punjab, and passes through Jhelum District. It is a tributary of the Indus River.
History
A photograph from 1900 shows a passenger traversing the river precariously seated in a small suspended cradle.
The river Jhelum was called Vitasta by the ancient Indians in the Vedic period and Hydaspes by the ancient Greeks. The Vitastā is mentioned as one of the major river by the holy scriptures of the Indo-Aryans—the Rigveda. It has been speculated that the Vitasta must have been one of the seven rivers (sapta-sindhu) mentioned so many times in the Rigveda. The name survives the a Kashmiri name for this river as Vyath.
The river was regarded as a god by the ancient Greeks, as were most mountains and streams; the poet Nonnus in the Dionysiaca (section 26, line 350) makes the Hydaspes a titan-descended god, the son of the sea-god Thaumas and the cloud-goddess Elektra. He was the brother of Iris the goddess of the rainbow, and half-brother to the harpies, the snatching winds. Since the river is in a country foreign to the ancient Greeks, it is not clear whether they named the river after the god, or whether the god Hydaspes was named after the river.
Alexander the Great and his army crossed the Jhelum in 326 BC at the Battle of the Hydaspes where he defeated the Indian king, Porus. According to Arrian (Anabasis, 29), he built a city "on the spot whence he started to cross the river Hydaspes", which he named Bukephala (or Bucephala) to honour his famous horse Bukephalis which was buried in Jalalpur Sharif. It is thought that ancient Bukephala was near the site of modern Jhelum City. According to a historian of Gujrat district,Mansoor Behzad Butt, Bukephala was buried in Jalalpur Sharif, but the people of Mandi Bahauddin, a district close to Jehlum, believed that their tehsil Phalia was named after Bucephala, Alexander`s dead horse. They say that the name Phalia was the distortion of the word Bucephala. The waters of the Jhelum are allocated to Pakistan under the terms of the Indus Waters Treaty.
Course
The river Jhelum rises from north-eastern Jammu and Kashmir and is fed by glaciers, and then passes through the Srinagar district. At the city of Srinagar, the serpentine Jhelum, along with the lake Dal which lies in its course, presents a very picturesque site. The Kishenganga(Neelum)River, the largest tributary of the Jhelum, joins it near Muzaffarabad, as does the next largest, the Kunhar River of the Kaghan valley.It also connects with Pakistan and Pakistan-held Kashmir on Kohala Bridge east of Circle Bakote. It is then joined by the Poonch river, and flows into the Mangla Dam reservoir in the district of Mirpur. The Jhelum enters the Punjab in the Jhelum District. From there, it flows through the plains of Pakistan's Punjab, forming the boundary between the Chaj and Sindh Sagar Doabs. It ends in a confluence with the Chenab at Trimmu in District Jhang. The Chenab merges with the Sutlej to form the Panjnad River which joins the Indus River at Mithankot.
Dams and Barrages
Mangla Dam, completed in 1967, is one of the largest earthfill dams in the world, with a storage capacity of 5.9 million acre-feet (7.3 km³)
Rasul Barrage, constructed in 1967, has a maximum flow of 850,000 ft³/s (24,000 m³/s).
Trimmu Barrage, constructed in 1939 at the confluence with the Chenab, has maximum discharge capacity of 645,000 ft³/s (18,000 m³/s).
Canals
The Upper Jhelum Canal runs from Mangla to the Chenab.
The Rasul-Qadirabad Link Canal runs from the Rasul barrage to the Chenab.
The Chashma-Jhelum Link Canal runs from the Chashma Barrage on the Indus River to the Jhelum river downstream of Rasul Barrage.
Kabul River
Kabul River or Kabal River is a river that rises in the Sanglakh Range of Afghanistan, separated from the watershed of the Helmand by the Unai Pass. It is the main river in the eastern part of Afghanistan. It flows 700 km before joining the Indus River near Attock . It passes through the cities of Kabul, Chaharbagh, Jalalabad, and (flowing into Pakistan some 30 km north of the Khyber Pass) Nowshera. The major tributaries of the Kabul River are the Logar, Panjshir, Kunar and Alingar rivers.
The Kabul river itself is little more than a trickle for most of the year, but swells in summer due to melting snows. Its largest tributary is the Kunar, which starts out as the Mastuj River, flowing from the Chiantar glacier in Chitral, Pakistan and once it flows south into Afghanistan it is met by the Bashgal river flowing from Nurestan. The Kunar meets the Kabul near Jalalabad. In spite of the Kunar carrying more water than the Kabul, the river continues as the Kabul River after this confluence, mainly for the political and historical significance of the name.
This river is attested in the Rig Veda, the earliest scripture of Hinduism, under the name Kubhā (many of the rivers of Afghanistan are mantioned in the Rig Veda). The Sanskrit word later changed to Kābul.
Swaan River
The Swaan River is the most important stream of the Pothohar region of Pakistan. It drains much of the water of Pothohar. It starts near a small village Bun in the foothills of Patriata and Murree. It provides water to Simlbee Dam, which is reservoir of water for Islamabad. Near Pharwala Fort it cuts through a high mountain range and that is a wonderful phenomenon of nature. The place is called Swan Cut. No stream can cut such a high mountain. It proves the Swaan was there before the formation of this range. And when the mountain rose through millions of years, the stream continued its path by cutting the rising mountain. Ling stream, following a relatively long course though Lehtrar and Kahuta falls in the Swaan near Sihala.
Islamabad Highway crosses this stream near Sihala where famous bridge Cock Pull is constructed over it. Another famous, Lai stream joins this stream near Swaan Camp. After walking a tortuous path and creating a big curve, the stream reaches Kalabagh where it falls into the Indus river. This relatively small stream is more than 250 kilometers long. Due to its mountainous course and shallow bed, it is hardly used for irrigation purposes. For grinding wheat, you can find ancient types of flour mills near Chakian.Fishing is not possible in this stream as a profession. Rohu is the main species of fish in this stream.
Kundar River
Kundar River is located in Balochistan, Pakistan. The meltwater from the Sulaiman Mountains forms Kundar River and it flows through Balochistan and drains into Gomal River.
The two principal drainage channels of the Zhob district are the Zhob River and the Kundar River, both flow into the Gomal River. The general direction of the rivers is from Southwest to northeast. The Zhob River rises at Tsari Mehtarazai pass, the watershed a distance of about 400 kilometers. The broad plain of the Zhob River is occupied by the alluvial formation. The Kundar River rises from the central and highest point of the TobaKakar range, a few kilometers northeast of the Sakir. It constitutes boundary between Pakistan and Afghanistan territory for a considerable length. The other subsidiary rivers or streams are the Baskan, Chukhan, Sri Toi, Sawar, Surab, etc.
Kunhar River
Kunhar River is located in North-West Frontier Province, Pakistan. A main source of the river is Lulusar lake, nearly 48km from Naran Valley. Glaciers of Malka Parbat and Makra Peak and the waters of Saiful Muluk lake feed the river. The Kunhar flows through the entire Kaghan Valley through Jalkhand, Naran, Kaghan, Jared, Paras and Balakot, and joins the Jhelum River.
The Kunhar river trout is considered to be the best throughout the sub-continent
Kurram River
The Kurrum River flows in the Kurrum Valley, stretching across the Afghan-Pakistani border west to east (crosses from the Paktia Province of Afghanistan into the Kohat border region of Pakistan) at 33°49′N 69°58′E, about 150 km west-to-south-west of the Khyber Pass.
The Kurram Agency is part of the Peshāwar Division of the Northwest Frontier Province. The Kurram River drains the southern flanks of the Safed Koh (Range), and enters the plains a north of Bannu, and joins the Indus River at 32°35′N 71°27′E near Isa Khel after a course of more than 320 km (200 miles). The district has an area of 3,310 km² (1,278 sq miles); pop. approx. 300,000. It lies between the Miranzai Valley and the Afghan border, and is inhabited by the Turis, a tribe of Turki and Parthian origin who are supposed to have subjugated the Bangash Pathans about six hundred years ago.
It is highly irrigated, well peopled, and crowded with small fortified villages, orchards and groves, to which a fine background is afforded by the dark pine forests and alpine snows of the Safed Koh. The beauty and climate of the valley attracted some of the Mogul emperors of Delhi, and the remains exist of a garden planted by Shah Jahan.
The Kurram River crosses the Afghan-Pakistan border about 80 km southwest of Jalalabad and in ancient times offered the most direct route to Kabul and Gardez. The route crossed the Peiwar Pass 3,439 m (11,283 ft) high, just over 20 km west of Parachinar, which was blocked by snow for several months of the year.
Formerly the Kurram Valley was under the government of Kabul, and every five or six years a military expedition was sent to collect the revenue, the soldiers living meanwhile at free quarters on the people. It was not until about 1848 that the Turis were brought directly under the control of Kabul, when a governor was appointed, who established himself in Kurram. The Turis, being Shiah Muslims, never liked the Afghan rule.
During the second Afghan War, when Sir Frederick Roberts advanced by way of the Kurram Valley and the Peiwar Kotal to Kabul, the Turis lent him every assistance in their power, and in consequence their independence was granted them in 1880.
The administration of the Kurram Valley was finally undertaken by the British government, at the request of the Turis themselves, in 1890. Technically it ranked, not as a British district, but as an agency or administered area.
Two expeditions in the Kurram Valley also require mention:
(1) The Kurram expedition of 1856 under Brigadier-General Sir Neville Chamberlain. The Turis on the first annexation of the Kohat district by the British had given much trouble. They had repeatedly leagued with other tribes to harry the Miranzai valley, harbouring fugitives, encouraging resistance, and frequently attacking Bangash and Khattak villages in the Kohat district. Accordingly, in 1856 a British force of 4,896 troops traversed their country, and the tribe entered into engagements for future good conduct.
(2) The Kohat-Kurram expedition of 5,897 under Colonel W. Hill. During the frontier risings of 1897 the inhabitants of the Kurram valley, chiefly the Massozai section of the Orakzais, were infected by the general excitement, and attacked the British camp at Sadda and other posts. A force of 14,230 British troops traversed the country, and the tribesmen were severely punished. In Lord Curzon's reorganization of the frontier in 1900-1901, the British troops were withdrawn from the forts in the Kurram Valley, and were replaced by the Kurram militia, reorganized in two battalions, and chiefly drawn from the Turi tribe.
In recent years the Kurram Valley has once again assumed a very strategic position and has been an area of intense military activity between the Taliban and American and allied forces.
Lyari River
Lyari River is located in Karachi, Sindh, Pakistan. Lyari River passes through the city of Karachi from north east to the center and drains into the Arabian Sea. Lyari river is one of the two rivers passing through Karachi and the other is Malir River.
Malir River
Malir River is located in Karachi, Sindh, Pakistan. Malir River passes through the city of Karachi from northeast to the centre and drains into the Arabian Sea. Malir river is one of the two rivers passing through Karachi and the other is Lyari River.it has two other little river help one is Thadho and other is Sukhan.In a rainy season this river flow with lot of water and millions of gallons of water waste in Arabian Sea. If the goverment becomes searious to this matter and construct a dam on this river, it will benefit the whole of Karachi a great deal.
Panjkora
The Panjkora River rises rises high in the Hindu Kush at lat. 35.45 and joins the Swat River near Chakdara, Malakand, NWFP, Pakistan. Its name is derived from the Persian for 'panj' (meaning 'five') and 'kora' (meaning 'river').
Panjnad River
Panjnad River (panj = five, nadi = river) is a river in Punjab, Pakistan. Panjnad River is formed by successive confluence of the five rivers of Punjab, namely Jhelum, Chenab, Ravi, Beas and Sutlej. Jhelum and Ravi join Chenab, Beas joins Sutlej, and then Sutlej and Chenab join to form Panjnad near Uch Sharif. The combined stream runs southwest for approximately 45 miles and joins Indus River at Mithankot. The Indus continues into the Arabian Sea. A dam on Panjnad has been erected; it provides irrigation channels for Punjab and Sind provinces south of the Sutlej and east of the Indus rivers.
Beyond the confluence of Indus and Panjnad rivers, the Indus river was known as Satnad (Sat = seven) carrying the waters of seven rivers including Indus river, Kabul river and the five rivers of Punjab.
Ravi River
The Ravi River is a river in India and Pakistan. It is one of the five rivers which give Punjab its name. The Ravi was known as Parushani or Iravati to Indians in Vedic times and Hydraotes to the Ancient Greeks. It originates in the Himalayas in the Chamba district of Himachal Pradesh following a north-westerly course. It turns to the south-west, near Dalhousie, and then cuts a gorge in the Dhaola Dhar range entering the Punjab plain near Madhopur. It then flows along the Indo-Pak border for some distance before entering Pakistan and joining the Chenab river. The total length of the river is about 720 km. The waters of the Ravi river are allocated to India under the Indus Waters Treaty between India and Pakistan. It is also called 'The river of Lahore' since that great city is located on its eastern bank. On its western bank is located the famous tomb of Jahangir.
Rig Veda
Part of the battle of the ten kings was fought on the Parushani river, which according to Yaska (nirukta 9.26) refers to the Iravati river (Ravi River) in the Punjab. Macdonell and Keith write that "the name [Parusni] is certainly that of the river later called Ravi (Iravati)"
Shigar River
Shigar River is located in Baltistan, Northern Areas, Pakistan. The Shigar River is formed from the melt water of the Baltoro Glacier and Biafo Glacier. The river is tributary to Indus River and meets the Indus in Skardu valley.
Sutlej River
Sutlej River (also known as Satluj), is the longest of the five rivers that flow through Indian Punjab in northern India. Its source is in Tibet near Mount Kailash and its terminus in Pakistani Punjab. It is the easternmost afluent of the Punjab, and it receives the Beas River in the state of Punjab, India and continues into Pakistan to join the Chenab River to form the Panjnad River, which further down its course joins the Indus River at Mithankot.
The Sutlej was known as Shatadru or Suṭudri to Indians in Vedic period and Zaradros or Hesidros to the Greeks, and Sydrus to the Romans.
The waters of the river are allocated to India under the Indus Waters Treaty between India and Pakistan. At present, most of its water is diverted to irrigation canals and used up in India. The Bhakra-Nangal Dam is a huge multipurpose dam on the river.
There is substantial evidence to indicate that prior to 1700 B.C. the Sutlej was once an important tributary of the Sarasvati River, instead of the Indus River. It is believed that tectonic activity created elevation changes that redirected the Sutlej from southeast to southwest. Once flowing in its new westward direction, the river eventually joined the Beas river. As a result, the mighty Sarasvati River began to dry up, causing the desertification of Cholistan and Sindh, as well as the abandonment of numerous ancient human settlements along its banks.
A canal is being built between the Sutlej and Yamuna rivers, known as the SLY.
Swat River
Swat River flows from Hindukush Mountains through Kalam valley and merges into Kabul River in peshawer valley Sarhad, Pakistan.
Swat River irrigates vast area of Swat District and contributes to fishing industry of the region. Saidu Group's of teaching hospitals also located at the banks of Swat River. Malamjaba ski resort is about 10 miles away from the river. Ayub Bridge is one of the attractions for visitors. The scenery attracts many tourists from all over Pakistan during the summer.
It is said that Alexander the Great crossed the Swat River with part of his army and before turning south to subdue the locals at what are now Barikoot and Odegram. Also, the banks of this river, which was earliest known as Shrivastu, later Suvastu and currently the present name, is the place of origin of the Shrivastava sub-clan of the Indo-Aryan Kayastha clan
Some 30 years ago, the water was fit for drinking even in Mingora (100 km downstream from Kalam), but now it is not safe even in Kalam.
Tochi river
Tochi river is located in North Waziristan, Federally Administered Tribal Areas, Pakistan. Tochi river flows eastward, in North Waziristan, to join the Kurram River and the Indus. It surrounds Waziristan in the North while the Gomal River river surrounds South Waziristan.
It is also sometimes referred to as the Gambila River.
Zhob River
Zhob River is located in Balochistan, Pakistan. The meltwater from the Sulaiman Mountains forms Zhob Rivers and it flows through Balochistan and drains into Gomal River. Zhob city is located on banks of Zhob river.
The two principal drainage channels of the Zhob district are the Zhob River and the Kundar River, both flow into the Gomal River. The general direction of the rivers is from Southwest to northeast. The Zhob River rises at Tsari Mehtarazai pass, the watershed a distance of about 400 kilometers. The broad plain of the Zhob River is occupied by the alluvial formation. The Kundar River rises from the central and highest point of the TobaKakar range, a few kilometers northeast of the Sakir. It constitutes boundary between Pakistan and Afghanistan territory for a considerable length. The other subsidiary rivers or streams are the Baskan, Chukhan, Sri Toi, Sawar, Surab, etc.
