Ghaggar-Hakra River
Encyclopedia
The Ghaggar-Hakra River (Devnagri: घग्गर हकरा, Gurmukhi: ਘੱਗਰ ਹਕਰਾ, Shahmukhi: گهگـر هکره) 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
and as the Hakra downstream of the barrage. The Ghaggar-Hakra is generally identified with the Vedic Sarasvati River by most scholars, though it is disputed whether all Rigvedic
references to the Sarasvati should be taken to refer to this river. The identification of the Vedic Sarasvati River with the Ghaggar-Hakra River was accepted by Christian Lassen
, Max Müller
, Marc Aurel Stein
, C.F. Oldham, and Jane Macintosh.
in India
, flowing during the monsoon
rain
s. It originates in the Shivalik Hills of Himachal Pradesh
and flows through Punjab and Haryana
states into Rajasthan
; just southwest of Sirsa, Haryana and by the side of talwara jheel
in Rajasthan
, this seasonal river feeds two irrigation canals that extend into Rajasthan
.
The present-day Sarsuti (Saraswati River) originates in a submontane region (Ambala
district) and joins the Ghaggar near Shatrana in Punjab. Near Sadulgarh (Hanumangarh) the Naiwal channel, a dried out channel of the Sutlej
, joins the Ghaggar. Near Suratgarh the Ghaggar is then joined by the dried up Drishadvati (Chautang) river.
The wide river bed (paleo-channel) of the Ghaggar river suggest that the river once flowed full of water during the great meltdown of the Himalayan Ice Age glaciers, some 10,000 years ago, and that it then 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
system and the Yamuna
river, and later on, additionally, the loss of water in much of its catchment area due to deforestation and overgrazing. This is supposed by some to have happened at the latest in 1900 BCE, but actually took place 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. However, recent studies show that Bronze Age sediments from the glaciers of the Himalayas are missing along the Ghaggar-Hakra, indicating that the river did not or no longer have its sources in the high mountains.
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
.
in Pakistan
that is the continuation of the Ghaggar River in India
. Several times, but not continuously, it carried the water of the Sutlej during the Bronze Age period. Many settlements of the Indus Valley Civilisation have been found along and inside the river beds of the Ghaggar and Hakra rivers.
except the fourth. It is the only river with hymns entirely dedicated to it: RV 6.61, RV 7.95 and RV 7.96.It is mentioned as a divine and large river,which flows "from the mountains to the samudra," which some take as the Indian Ocean
. Talageri states that "the references to the Sarasvati far outnumber the references to the Indus" and "The Sarasvati is so important in the whole of the Rigveda that it is worshipped as one of the Three Great Goddesses". However, the reason for the predominance of the Sarasvati in the Rigveda is the late Harappan (1900-1300 BCE) population shift eastwards to Haryana; the latter part of the period corresponds to the common scholarly opinion of the date of this text.
Another reference to the Sarasvati is in the geographical enumeration of the rivers in the late Rigvedic Nadistuti sukta
(10.75.5, this verse enumerates all important rivers from the Ganges in the east up to the Indus in the west in a strict geographical order), as "Ganges, Yamuna
, Sarasvati, Shutudri", the Sarasvati is placed between the Yamuna and the Sutlej
, consistent with the Ghaggar identification. It is clear, therefore, that even if the river had unmistakably lost much of her former prominence, the Sarasvati remained characterized as a river goddess almost throughout the Rigveda.
According to some palaeo-environmental scientists and Archaeologists,between 2500 BCE and 1900 BCE some tectonic disturbances caused tilt in topography of Northwest India resulting in the migration of river. The Sutlej moved westward and became a tributary of the Indus River while the Yamuna moved eastward and became a tributary of the Ganges. The Yamuna shifted its course eastwards, supposedly in the early 2nd millennium BCE, allegedly reaching its current bed by 1st millennium BCE, while the Drishadvati bed retained only a small seasonal flow. The Sutlej several times over shifted its channel northwards and was eventually captured by the Indus system. The water loss due to these movements caused the Sarasvati river to dry up in the Thar Desert
.
However, Henri-Paul Francfort
, utilizing images from the French satellite SPOT
already two decades ago, found that the large river Sarasvati is pre-Harappan altogether and started drying up already in the middle of the 4th millennium BC; during Harappan times only a complex irrigation-canal network was being used. The date should therefore be pushed back to c 3800 BC. R. Mughal (1997), summing up the evidence, concludes that the Bronze Age Ghaggar-Hakra sometimes carried more, sometimes less water (for example derived from the Sutlej). The latter point agrees with a recent isotope study. Painted Grey Ware sites (ca. 1000 BCE) have been found in the river bed and not on the banks of the Ghaggar-Hakra river, which suggests that river was certainly dried up by this period.
The Rig Vedic hymn X 75, however, gives a list of names of rivers where Sarasvati is merely mentioned while Sindhu receives praise. It is commonly agreed that the tenth Book of the Rig Veda is later than the others. Some revisionists think, ahistorically, that this may indicate that the Rig Veda could be dated to a period after the first drying up of Sarasvati (c. 3500 BCE) when the river lost its preeminence.
Scholars, however, commonly date the Rig Veda to after the Indus Valley culture, arguing for example, that the lack of clear evidence of domesticated equids at Indus Valley culture sites contrasts with the Rig Veda's frequent references to domesticated horses. Scholars also interpret frequent use in the Rig Veda of the word "ratha", which in later Sanskrit can mean any kind of carriage, to be references specifically to horse-drawn, spoked-wheeled war chariots, whereas the only carts (called 'anas' in Vedic) found at Indus Valley culture sites are solid-wheeled bullock carts. There are indeed a number of mentions in the Rig Veda of spoked (ara) wheels, horse-drawn chariots and the use of chariots in sport, competition and battle, including also the deity Indra's vehicle. Indra is described as throwing his vajra weapon from a heavenly "ratha" pulled by two "hari" horses, a noun form of "bay".
The many archeological sites along the bed of Sarasvati (variously given as 414 or even 600) dwarf the number of sites so far recorded along the Indus River, which number less (about three dozen). However, most of the Harappan sites along the Sarasvati are found in desert country, and have remained undisturbed since the end of the Indus Civilization. This contrasts with the heavy alluvium of the Indus and other large Panjab rivers that have obscured Harappan sites, including part of Mohenjo Daro. About 80 percent of the Sarasvati sites are datable to the fourth or third millennium BCE, suggesting that the river was flowing during (part of) this period, which is also indicated by the fact that some Indus sites are found inside the bed of the Ghaggar-Hakra.
(2600 to 1900 BC) it makes all the difference whether the river dried up in 2500 (its early phase) or 2000 (its late phase). By contact with remnants of the IVC like the Cemetery H culture
, legendary knowledge of the event may have been acquired.
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 has been assumed that the Sarasvati ended there in a series of terminal lakes, and some think that its water only reached the Indus or the sea in very wet rainy seasons. However, satellite images contradict this: they do not show subterranean water in reservoirs in the dunes between the Indus and the end of the Hakra west of Fort Derawar/Marot. It may also have been affected by much of its water being taken for irrigation.
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.
S. P. Gupta however counts over 600 sites of the Indus civilization on the Ghaggar-Hakra river and its tributaries. For ereason stated above, 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 Late Harappan or OCP) are located on the Ghaggar-Hakra. The other sites are mainly in Kutch-Saurashtra (nearly 200 sites), Yamuna Valley (nearly 70 Late Harappan sites) and in the Indus Valley, in Baluchistan, and in the NW Frontier Province (less than 100 sites).
Most of the Mature Harappan sites are located in the middle Ghaggar-Hakra river valley, and some on the Indus and in Kutch-Saurashtra. However, just as in other contemporary cultures, such as the BMAC, settlements move up-river due to climate changes around 2000 BCE. In the late Harappan period the number of late Harappan sites in the middle Ghaggar-Hakra channel and in the Indus valley diminishes, while it expands in the upper Ghaggar-Sutlej channels and in Saurashtra. The abandonment of many sites on the Ghaggar-Hakra between the Harappan and the Late Harappan phase was probably due to the drying up of the Ghaggar-Hakra river.
Painted Grey Ware sites (ca. 1000 BCE) have been found in the bed and not on the banks of the Ghaggar-Hakra river.
Because most of the Indus Valley sites known so far are actually located on the Ghaggar-Hakra river and its tributaries and not on the Indus river, some Indian archaeologists, such as S.P. Gupta, have proposed to use the term "Indus Sarasvati Civilization" to refer to the Harappan culture which is named, as is common in archaeology, after the first place where the culture was discovered.
and possibly also the Yamuna
once flowed into the Ghaggar-Hakra river bed. The Sutlej and Yamuna Rivers have changed their courses several times.
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 additionally have been caused by earthquake
s 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 as well as deforestation and overgrazing may have also contributed to the drying up of the river. However, a similar phenomenon, caused by climate change, is also seen at about the same period north of the Hindu Kush, in the area of the Bactria-Margiana Archaeological Complex
.
At Ropar the Sutlej river suddenly turns sharply away from the Ghaggar. The narrow Ghaggar river bed itself is becoming suddenly wider at the conjunction where the Sutlej should have met the Ghaggar river. There also is a major paleochannel between the turning point of the Sutlej and where the Ghaggar river bed widens.
In later texts like the Mahabharata
, the Rigvedic Sutudri (of unknown, non-Sanskrit etymology) is called Shatudri (Shatadru/Shatadhara), which means a river with 100 flows. As mentioned, the Sutlej (and the Beas and Ravi) have frequently changed their courses. The Beas probably joined the Sutlej (as in Rgveda 3.33) further downstream from where it joins that river today. Before that time, the Sutlej is said to have flowed into Ghaggar.
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 flowed into the Sarasvati during Harappan times. There are several 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 flowed into the Sarasvati river through the Chautang
or the Drishadvati channel, since many Harappan sites have been discovered on these dried out river beds.
is based the mentionings in Vedic texts (e.g. in the enumeration of the rivers in Rigveda 10.75
.05 - the order is Ganges, Yamuna
, Sarasvati, Sutudri Sutlej
), Parusni, etc. - and other geological and paleobotanical findings. This however, is disputed. The Victorian era
scholar C.F. Oldham (1886) was the first to suggest that geological events had redirected the river, and to connect it to the lost Sarasvati: "[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." It also is alleged 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.
India
India , officially the Republic of India , is a country in South Asia. It is the seventh-largest country by geographical area, the second-most populous country with over 1.2 billion people, and the most populous democracy in the world...
and Pakistan
Pakistan
Pakistan , officially the Islamic Republic of Pakistan is a sovereign state in South Asia. It has a coastline along the Arabian Sea and the Gulf of Oman in the south and is bordered by Afghanistan and Iran in the west, India in the east and China in the far northeast. In the north, Tajikistan...
that flows only during the monsoon
Monsoon
Monsoon is traditionally defined as a seasonal reversing wind accompanied by corresponding changes in precipitation, but is now used to describe seasonal changes in atmospheric circulation and precipitation associated with the asymmetric heating of land and sea...
season. The river is known as Ghaggar before the Ottu barrage
Ottu barrage
The Ottu barrage , sometimes spelled as the Otu barrage and also known as Ottu Head, is a masonry weir on the Ghaggar-Hakra river in Haryana state of India that creates a large water reservoir out of the formerly-small Dhanur lake, located near the village of Ottu, which is about 8 miles from Sirsa...
and as the Hakra downstream of the barrage. The Ghaggar-Hakra is generally identified with the Vedic Sarasvati River by most scholars, though it is disputed whether all Rigvedic
Rigveda
The Rigveda is an ancient Indian sacred collection of Vedic Sanskrit hymns...
references to the Sarasvati should be taken to refer to this river. The identification of the Vedic Sarasvati River with the Ghaggar-Hakra River was accepted by Christian Lassen
Christian Lassen
Christian Lassen was a Norwegian-German orientalist.-Life:He was born at Bergen, Norway. Having received a university education at Oslo, he went to Germany and continued his studies at the University of Heidelberg and the University of Bonn. In Bonn, Lassen acquired a sound knowledge of Sanskrit...
, Max Müller
Max Müller
Friedrich Max Müller , more regularly known as Max Müller, was a German philologist and Orientalist, one of the founders of the western academic field of Indian studies and the discipline of comparative religion...
, Marc Aurel Stein
Marc Aurel Stein
Sir Marc Aurel Stein KCIE, FBA was a Hungarian archaeologist, primarily known for his explorations and archaeological discoveries in Central Asia. He was also a professor at various Indian universities.-Early life:Stein was born in Budapest into a Jewish family...
, C.F. Oldham, and Jane Macintosh.
Ghaggar River
The Ghaggar is an intermittent riverRiver
A river is a natural watercourse, usually freshwater, flowing towards an ocean, a lake, a sea, or another river. In a few cases, a river simply flows into the ground or dries up completely before reaching another body of water. Small rivers may also be called by several other names, including...
in India
India
India , officially the Republic of India , is a country in South Asia. It is the seventh-largest country by geographical area, the second-most populous country with over 1.2 billion people, and the most populous democracy in the world...
, flowing during the monsoon
Monsoon
Monsoon is traditionally defined as a seasonal reversing wind accompanied by corresponding changes in precipitation, but is now used to describe seasonal changes in atmospheric circulation and precipitation associated with the asymmetric heating of land and sea...
rain
Rain
Rain is liquid precipitation, as opposed to non-liquid kinds of precipitation such as snow, hail and sleet. Rain requires the presence of a thick layer of the atmosphere to have temperatures above the melting point of water near and above the Earth's surface...
s. It originates in the Shivalik Hills of Himachal Pradesh
Himachal Pradesh
Himachal Pradesh is a state in Northern India. It is spread over , and is bordered by the Indian states of Jammu and Kashmir on the north, Punjab on the west and south-west, Haryana and Uttar Pradesh on the south, Uttarakhand on the south-east and by the Tibet Autonomous Region on the east...
and flows through Punjab and Haryana
Haryana
Haryana is a state in India. Historically, it has been a part of the Kuru region in North India. The name Haryana is found mentioned in the 12th century AD by the apabhramsha writer Vibudh Shridhar . It is bordered by Punjab and Himachal Pradesh to the north, and by Rajasthan to the west and south...
states into Rajasthan
Rajasthan
Rājasthān the land of Rajasthanis, , is the largest state of the Republic of India by area. It is located in the northwest of India. It encompasses most of the area of the large, inhospitable Great Indian Desert , which has an edge paralleling the Sutlej-Indus river valley along its border with...
; just southwest of Sirsa, Haryana and by the side of talwara jheel
Talwara lake
Talwara Lake is a small seasonal lake that forms in a depression along the course of the Ghaggar-Hakra River in Hanumangarh district of Rajasthan state of India. In his invasion of India in 1398-99 CE, Timur encamped at the banks of this lake after overpowering Bhatnair Fort in modern-day...
in Rajasthan
Rajasthan
Rājasthān the land of Rajasthanis, , is the largest state of the Republic of India by area. It is located in the northwest of India. It encompasses most of the area of the large, inhospitable Great Indian Desert , which has an edge paralleling the Sutlej-Indus river valley along its border with...
, this seasonal river feeds two irrigation canals that extend into Rajasthan
Rajasthan
Rājasthān the land of Rajasthanis, , is the largest state of the Republic of India by area. It is located in the northwest of India. It encompasses most of the area of the large, inhospitable Great Indian Desert , which has an edge paralleling the Sutlej-Indus river valley along its border with...
.
The present-day Sarsuti (Saraswati River) originates in a submontane region (Ambala
Ambala
Ambala is a city and a municipal corporation in Ambala district in the state of Haryana, India, located on the border of the states of Haryana and Punjab in India. Politically; Ambala has two sub-areas: Ambala Cantt and Ambala City, approximately 3 kilometers apart from each other...
district) and joins the Ghaggar near Shatrana in Punjab. Near Sadulgarh (Hanumangarh) the Naiwal channel, a dried out channel of the Sutlej
Sutlej
The Sutlej River is the longest of the five rivers that flow through the historic crossroad region of Punjab in northern India and Pakistan. It is located north of the Vindhya Range, south of the Hindu Kush segment of the Himalayas, and east of the Central Sulaiman Range in Pakistan.The Sutlej...
, joins the Ghaggar. Near Suratgarh the Ghaggar is then joined by the dried up Drishadvati (Chautang) river.
The wide river bed (paleo-channel) of the Ghaggar river suggest that the river once flowed full of water during the great meltdown of the Himalayan Ice Age glaciers, some 10,000 years ago, and that it then continued through the entire region, in the presently dry channel of the Hakra River, possibly emptying into the Rann of Kutch
Rann of Kutch
The Great Rann of Kutch, also called Greater Rann of Kutch or just Rann of Kutch , is a seasonal salt marsh located in the Thar Desert in the Kutch District of Gujarat, India and the Sindh province of Pakistan....
. It supposedly dried up due to the capture of its tributaries by the Indus
Indus River
The Indus River is a major river which flows through Pakistan. It also has courses through China and India.Originating in the Tibetan plateau of western China in the vicinity of Lake Mansarovar in Tibet Autonomous Region, the river runs a course through the Ladakh district of Jammu and Kashmir and...
system and the Yamuna
Yamuna
The Yamuna is the largest tributary river of the Ganges in northern India...
river, and later on, additionally, the loss of water in much of its catchment area due to deforestation and overgrazing. This is supposed by some to have happened at the latest in 1900 BCE, but actually took place much earlier
Puri and Verma (1998) have argued that the present-day Tons River
Tons River
The Tons is the largest tributary of the Yamuna and flows through Garhwal region in Uttarakhand, touching Himachal Pradesh. The Tons thrust is named after this 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. However, recent studies show that Bronze Age sediments from the glaciers of the Himalayas are missing along the Ghaggar-Hakra, indicating that the river did not or no longer have its sources in the high mountains.
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
Aravalli Range
The Aravalli Range literally meaning 'line of peaks', is a range of mountains in western India and eastern Pakistan running approximately 800 km from northeast to southwest across states of Rajasthan, Haryana, and Gujarat and Pakistani provinces of Punjab and Sindh...
into the east end of the Rann of Kutch
Rann of Kutch
The Great Rann of Kutch, also called Greater Rann of Kutch or just Rann of Kutch , is a seasonal salt marsh located in the Thar Desert in the Kutch District of Gujarat, India and the Sindh province of Pakistan....
.
Hakra River
The Hakra is the dried-out channel of a riverRiver
A river is a natural watercourse, usually freshwater, flowing towards an ocean, a lake, a sea, or another river. In a few cases, a river simply flows into the ground or dries up completely before reaching another body of water. Small rivers may also be called by several other names, including...
in Pakistan
Pakistan
Pakistan , officially the Islamic Republic of Pakistan is a sovereign state in South Asia. It has a coastline along the Arabian Sea and the Gulf of Oman in the south and is bordered by Afghanistan and Iran in the west, India in the east and China in the far northeast. In the north, Tajikistan...
that is the continuation of the Ghaggar River in India
India
India , officially the Republic of India , is a country in South Asia. It is the seventh-largest country by geographical area, the second-most populous country with over 1.2 billion people, and the most populous democracy in the world...
. Several times, but not continuously, it carried the water of the Sutlej during the Bronze Age period. Many settlements of the Indus Valley Civilisation have been found along and inside the river beds of the Ghaggar and Hakra rivers.
Palaeogeography
The Sarasvati River is mentioned in all books of the RigvedaRigveda
The Rigveda is an ancient Indian sacred collection of Vedic Sanskrit hymns...
except the fourth. It is the only river with hymns entirely dedicated to it: RV 6.61, RV 7.95 and RV 7.96.It is mentioned as a divine and large river,which flows "from the mountains to the samudra," which some take as the Indian Ocean
Indian Ocean
The Indian Ocean is the third largest of the world's oceanic divisions, covering approximately 20% of the water on the Earth's surface. It is bounded on the north by the Indian Subcontinent and Arabian Peninsula ; on the west by eastern Africa; on the east by Indochina, the Sunda Islands, and...
. Talageri states that "the references to the Sarasvati far outnumber the references to the Indus" and "The Sarasvati is so important in the whole of the Rigveda that it is worshipped as one of the Three Great Goddesses". However, the reason for the predominance of the Sarasvati in the Rigveda is the late Harappan (1900-1300 BCE) population shift eastwards to Haryana; the latter part of the period corresponds to the common scholarly opinion of the date of this text.
Another reference to the Sarasvati is in the geographical enumeration of the rivers in the late Rigvedic Nadistuti sukta
Nadistuti sukta
The Nadistuti sukta ,"hymn of praise of rivers", is hymn 10.75 of the Rigveda.It is important for the reconstruction of the geography of the Vedic civilization...
(10.75.5, this verse enumerates all important rivers from the Ganges in the east up to the Indus in the west in a strict geographical order), as "Ganges, Yamuna
Yamuna
The Yamuna is the largest tributary river of the Ganges in northern India...
, Sarasvati, Shutudri", the Sarasvati is placed between the Yamuna and the Sutlej
Sutlej
The Sutlej River is the longest of the five rivers that flow through the historic crossroad region of Punjab in northern India and Pakistan. It is located north of the Vindhya Range, south of the Hindu Kush segment of the Himalayas, and east of the Central Sulaiman Range in Pakistan.The Sutlej...
, consistent with the Ghaggar identification. It is clear, therefore, that even if the river had unmistakably lost much of her former prominence, the Sarasvati remained characterized as a river goddess almost throughout the Rigveda.
According to some palaeo-environmental scientists and Archaeologists,between 2500 BCE and 1900 BCE some tectonic disturbances caused tilt in topography of Northwest India resulting in the migration of river. The Sutlej moved westward and became a tributary of the Indus River while the Yamuna moved eastward and became a tributary of the Ganges. The Yamuna shifted its course eastwards, supposedly in the early 2nd millennium BCE, allegedly reaching its current bed by 1st millennium BCE, while the Drishadvati bed retained only a small seasonal flow. The Sutlej several times over shifted its channel northwards and was eventually captured by the Indus system. The water loss due to these movements caused the Sarasvati river to dry up in the Thar Desert
Thar Desert
The Thar Desert |Punjab]] province. The Cholistan Desert adjoins the Thar desert spreading into Pakistani Punjab province.-Location and description:...
.
However, Henri-Paul Francfort
Henri-Paul Francfort
Henri-Paul Francfort is a French archaeologist and member of the CNRS. He is noted for his excavations at Shortugai.- Publications :...
, utilizing images from the French satellite SPOT
SPOT (satellites)
SPOT is a high-resolution, optical imaging Earth observation satellite system operating from space. It is run by Spot Image based in Toulouse, France...
already two decades ago, found that the large river Sarasvati is pre-Harappan altogether and started drying up already in the middle of the 4th millennium BC; during Harappan times only a complex irrigation-canal network was being used. The date should therefore be pushed back to c 3800 BC. R. Mughal (1997), summing up the evidence, concludes that the Bronze Age Ghaggar-Hakra sometimes carried more, sometimes less water (for example derived from the Sutlej). The latter point agrees with a recent isotope study. Painted Grey Ware sites (ca. 1000 BCE) have been found in the river bed and not on the banks of the Ghaggar-Hakra river, which suggests that river was certainly dried up by this period.
The Rig Vedic hymn X 75, however, gives a list of names of rivers where Sarasvati is merely mentioned while Sindhu receives praise. It is commonly agreed that the tenth Book of the Rig Veda is later than the others. Some revisionists think, ahistorically, that this may indicate that the Rig Veda could be dated to a period after the first drying up of Sarasvati (c. 3500 BCE) when the river lost its preeminence.
Scholars, however, commonly date the Rig Veda to after the Indus Valley culture, arguing for example, that the lack of clear evidence of domesticated equids at Indus Valley culture sites contrasts with the Rig Veda's frequent references to domesticated horses. Scholars also interpret frequent use in the Rig Veda of the word "ratha", which in later Sanskrit can mean any kind of carriage, to be references specifically to horse-drawn, spoked-wheeled war chariots, whereas the only carts (called 'anas' in Vedic) found at Indus Valley culture sites are solid-wheeled bullock carts. There are indeed a number of mentions in the Rig Veda of spoked (ara) wheels, horse-drawn chariots and the use of chariots in sport, competition and battle, including also the deity Indra's vehicle. Indra is described as throwing his vajra weapon from a heavenly "ratha" pulled by two "hari" horses, a noun form of "bay".
The many archeological sites along the bed of Sarasvati (variously given as 414 or even 600) dwarf the number of sites so far recorded along the Indus River, which number less (about three dozen). However, most of the Harappan sites along the Sarasvati are found in desert country, and have remained undisturbed since the end of the Indus Civilization. This contrasts with the heavy alluvium of the Indus and other large Panjab rivers that have obscured Harappan sites, including part of Mohenjo Daro. About 80 percent of the Sarasvati sites are datable to the fourth or third millennium BCE, suggesting that the river was flowing during (part of) this period, which is also indicated by the fact that some Indus sites are found inside the bed of the Ghaggar-Hakra.
Association with the Harappan civilization
Some estimate that the 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 mature Indus Valley CivilizationIndus Valley Civilization
The Indus Valley Civilization was a Bronze Age civilization that was located in the northwestern region of the Indian subcontinent, consisting of what is now mainly modern-day Pakistan and northwest India...
(2600 to 1900 BC) it makes all the difference whether the river dried up in 2500 (its early phase) or 2000 (its late phase). By contact with remnants of the IVC like the Cemetery H culture
Cemetery H culture
The Cemetery H culture developed out of the northern part of the Indus Valley Civilization around 1900 BCE, in and around western Punjab region located in present-day India and Pakistan...
, legendary knowledge of the event may have been acquired.
Along the course of the Ghaggar-Hakra river are many archaeological sites of the Indus Valley Civilization
Indus Valley Civilization
The Indus Valley Civilization was a Bronze Age civilization that was located in the northwestern region of the Indian subcontinent, consisting of what is now mainly modern-day Pakistan and northwest India...
; but not further south than the middle of Bahawalpur
Bahawalpur
Bahawalpur , located in the province of Punjab, is the twelfth largest city in Pakistan. The city was once the capital of the former princely state of Bahawalpur. The city was home to various Nawabs and counted as part of the Rajputana states...
district. It has been assumed that the Sarasvati ended there in a series of terminal lakes, and some think that its water only reached the Indus or the sea in very wet rainy seasons. However, satellite images contradict this: they do not show subterranean water in reservoirs in the dunes between the Indus and the end of the Hakra west of Fort Derawar/Marot. It may also have been affected by much of its water being taken for irrigation.
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.
S. P. Gupta however counts over 600 sites of the Indus civilization on the Ghaggar-Hakra river and its tributaries. For ereason stated above, 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 Late Harappan or OCP) are located on the Ghaggar-Hakra. The other sites are mainly in Kutch-Saurashtra (nearly 200 sites), Yamuna Valley (nearly 70 Late Harappan sites) and in the Indus Valley, in Baluchistan, and in the NW Frontier Province (less than 100 sites).
Most of the Mature Harappan sites are located in the middle Ghaggar-Hakra river valley, and some on the Indus and in Kutch-Saurashtra. However, just as in other contemporary cultures, such as the BMAC, settlements move up-river due to climate changes around 2000 BCE. In the late Harappan period the number of late Harappan sites in the middle Ghaggar-Hakra channel and in the Indus valley diminishes, while it expands in the upper Ghaggar-Sutlej channels and in Saurashtra. The abandonment of many sites on the Ghaggar-Hakra between the Harappan and the Late Harappan phase was probably due to the drying up of the Ghaggar-Hakra river.
Painted Grey Ware sites (ca. 1000 BCE) have been found in the bed and not on the banks of the Ghaggar-Hakra river.
Because most of the Indus Valley sites known so far are actually located on the Ghaggar-Hakra river and its tributaries and not on the Indus river, some Indian archaeologists, such as S.P. Gupta, have proposed to use the term "Indus Sarasvati Civilization" to refer to the Harappan culture which is named, as is common in archaeology, after the first place where the culture was discovered.
Ancient tributaries
Satellite photography has shown that the Ghaggar-Hakra was indeed a large river that dried up several times (see Mughal 1997). The dried out Hakra river bed is between three and ten kilometers wide. Recent research indicates that the SutlejSutlej
The Sutlej River is the longest of the five rivers that flow through the historic crossroad region of Punjab in northern India and Pakistan. It is located north of the Vindhya Range, south of the Hindu Kush segment of the Himalayas, and east of the Central Sulaiman Range in Pakistan.The Sutlej...
and possibly also the Yamuna
Yamuna
The Yamuna is the largest tributary river of the Ganges in northern India...
once flowed into the Ghaggar-Hakra river bed. The Sutlej and Yamuna Rivers have changed their courses several times.
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 additionally have been caused by earthquake
Earthquake
An earthquake is the result of a sudden release of energy in the Earth's crust that creates seismic waves. The seismicity, seismism or seismic activity of an area refers to the frequency, type and size of earthquakes experienced over a period of time...
s 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 as well as deforestation and overgrazing may have also contributed to the drying up of the river. However, a similar phenomenon, caused by climate change, is also seen at about the same period north of the Hindu Kush, in the area of the Bactria-Margiana Archaeological Complex
Bactria-Margiana Archaeological Complex
The Bactria–Margiana Archaeological Complex is the modern archaeological designation for a Bronze Age culture of Central Asia, dated to ca. 2300–1700 BC, located in present day Turkmenistan, northern Afghanistan and northeastern Iran, southern Uzbekistan and western Tajikistan, centered on...
.
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 Ghaggar-Hakra at that time.At Ropar the Sutlej river suddenly turns sharply away from the Ghaggar. The narrow Ghaggar river bed itself is becoming suddenly wider at the conjunction where the Sutlej should have met the Ghaggar river. There also is a major paleochannel between the turning point of the Sutlej and where the Ghaggar river bed widens.
In later texts like the Mahabharata
Mahabharata
The Mahabharata is one of the two major Sanskrit epics of ancient India and Nepal, the other being the Ramayana. The epic is part of itihasa....
, the Rigvedic Sutudri (of unknown, non-Sanskrit etymology) is called Shatudri (Shatadru/Shatadhara), which means a river with 100 flows. As mentioned, the Sutlej (and the Beas and Ravi) have frequently changed their courses. The Beas probably joined the Sutlej (as in Rgveda 3.33) further downstream from where it joins that river today. Before that time, the Sutlej is said to have flowed into Ghaggar.
Yamuna
There are no Harappan sites on the present Yamuna river. There are however Painted Gray Ware (1000 - 600 BC) sites along the Yamuna channel, showing that the river must have then flowed in the present channel. The sparse 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 flowed into the Sarasvati during Harappan times. There are several 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
Yamuna
The Yamuna is the largest tributary river of the Ganges in northern India...
may have flowed into the Sarasvati river through the Chautang
Chautang
The Chautang river is a seasonal river in the state of Haryana, India. Some believe it to be remnant of the Drsadvati River mentioned in Vedas and the Mahabharata....
or the Drishadvati channel, since many Harappan sites have been discovered on these dried out river beds.
Identification with the Rigvedic Sarasvati
The identity of the dried-up Ghaggar-Hakra with the late Vedic and post-Vedic Sarasvati is widely accepted. The identification of the early Rigvedic Sarasvati with the Old Ghaggar is another matter, and the subject of recent dispute. The identification with the Sarasvati RiverSarasvati River
The Sarasvati River is one of the chief Rigvedic rivers mentioned in ancient Hindu texts. The Nadistuti hymn in the Rigveda mentions the Sarasvati between the Yamuna in the east and the Sutlej in the west, and later Vedic texts like Tandya and Jaiminiya Brahmanas as well as the Mahabharata...
is based the mentionings in Vedic texts (e.g. in the enumeration of the rivers in Rigveda 10.75
Nadistuti sukta
The Nadistuti sukta ,"hymn of praise of rivers", is hymn 10.75 of the Rigveda.It is important for the reconstruction of the geography of the Vedic civilization...
.05 - the order is Ganges, Yamuna
Yamuna
The Yamuna is the largest tributary river of the Ganges in northern India...
, Sarasvati, Sutudri Sutlej
Sutlej
The Sutlej River is the longest of the five rivers that flow through the historic crossroad region of Punjab in northern India and Pakistan. It is located north of the Vindhya Range, south of the Hindu Kush segment of the Himalayas, and east of the Central Sulaiman Range in Pakistan.The Sutlej...
), Parusni, etc. - and other geological and paleobotanical findings. This however, is disputed. The Victorian era
Victorian era
The Victorian era of British history was the period of Queen Victoria's reign from 20 June 1837 until her death on 22 January 1901. It was a long period of peace, prosperity, refined sensibilities and national self-confidence...
scholar C.F. Oldham (1886) was the first to suggest that geological events had redirected the river, and to connect it to the lost Sarasvati: "[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." It also is alleged 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.
- Between 2500 BCE and 1900 BCE,Some techtonic disturbances caused tilt in topography of Northwest India resulting in the migration of rivers. The Sutlej moved westward and became a tributary of the Indus River while the Yamuna moved eastward and became a tributary of the Ganges. The water loss due to these movements caused the river to dry up in the Thar Desert, without reaching the sea. Later Vedic texts record the river as disappearing at Vinasana (literally, "the disappearing") or Upamajjana, and in post-Vedic texts as joining both the Yamuna and Ganges as an invisible river at Prayaga (Allahabad). Some claim that the sanctity of the modern Ganges is directly related to its assumption of the holy, life-giving waters of the ancient Saraswati.
- The identification is also justified by post-Vedic literature like MahabharataMahabharataThe Mahabharata is one of the two major Sanskrit epics of ancient India and Nepal, the other being the Ramayana. The epic is part of itihasa....
.According to Adi Parvan of the Mahabharata(1.90.25-26),it is mentioned that "Many kings performed yajña (sacrifice) in Fire altars at the bank of Sarasvati riverSarasvati RiverThe Sarasvati River is one of the chief Rigvedic rivers mentioned in ancient Hindu texts. The Nadistuti hymn in the Rigveda mentions the Sarasvati between the Yamuna in the east and the Sutlej in the west, and later Vedic texts like Tandya and Jaiminiya Brahmanas as well as the Mahabharata...
, which is connected with the alleged Harappan fire altars at KalibanganKalibanganKalibangān is a town located at on the left or southern banks of the Ghaggar , identified by some scholars with Sarasvati River in Tehsil Pilibangān, between Suratgarh and Hanumāngarh in Hanumangarh district, Rajasthan, India 205 km. from Bikaner...
, a town located on the left or southern banks of the Ghaggar River. They are even assumed by some to be Vedic and that the structures may perhaps have been used for ritual purposes.
- The MahabharataMahabharataThe Mahabharata is one of the two major Sanskrit epics of ancient India and Nepal, the other being the Ramayana. The epic is part of itihasa....
says that the Sarasvati dried up in a desert (at a place named Vinasana or Adarsana). According to the Mahabharata, the river dried up in order that the Nishadas and Abhiras might not see her. The MahabharataMahabharataThe Mahabharata is one of the two major Sanskrit epics of ancient India and Nepal, the other being the Ramayana. The epic is part of itihasa....
also states that Vasishtha committed suicide by throwing himself into the Sutlej and that the Sutlej then broke up in a 100 channels (Yash Pal in S.P. Gupta 1995: 175). This myth seems to be related with the changing of the course of the Sutlej river. According to the Mahabharata (3.81.115), KurukshetraKurukshetraKurukshetra is a land of historical and religious importance. Historically the land belonged to Punjab now a district in Haryana state of India. It is a holy place and is also known as Dharmakshetra . According to the Puranas, Kurukshetra is named after King Kuru, the ancestor of Kauravas and...
is south of the Sarasvati and north of the Drishadvati. In the Sabha Parvan of the Mahabharata (2.29.8) it is mentioned that "Nakula conquered the Shudra and Abhira who lived at the bank of the Sarasvati near the Sindhu (Indus) river.