Ghaggar-Hakra River - Ghaggar River

Ghaggar River

The Ghaggar is an intermittent river in India, flowing during the monsoon rains. 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 Lake 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.

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