However, the lack of large-scale incision on the interfluve demonstrates that large, glacier-fed rivers did not flow across the Ghaggar-Hakra region during the Holocene. पाकिस्तान के घृणित मंसूबों को ध्वस्त कर रहे... दिवाली पर रात 10 बजे तक ही मिलेगी दिल्ली... पीएम मोदी की देशवासियों से अपील, दिवाली पर... इसे लेकर पहले भी एन.जी.टी. Yet, more recent research shows that the Ghaggar-Hakra was monsoon-fed during Harappan times, and had already dried-up during Vedic times. Punjab: Ghaggar river breach yet to be plugged, over 60,000 acres under rain, river water In Sangrur’s Moonak area, crops and tubewell motors in Moonak, Makror Sahib, Phoolad, Salemgarh, Surjan Bhaini and Sunder Bhaini villages are all under water due to the Ghaggar breach. [note 3][note 4] They concluded that the Indus Valley Civilisation died out because the monsoons, which fed the rivers that supported the civilisation, diminished. ध्रुमन एच. (2012), using dating of zircon sand grains, have shown that subsurface river channels near the Indus Valley Civilisation sites in Cholistan immediately below the dry Ghaggar-Hakra bed show sediment affinity not with the Ghagger-Hakra, but instead with the Beas River in the western sites and the Sutlej and the Yamuna in the eastern ones, further weakening the hypothesis that the Ghaggar-Hakra was once a large river, but suggesting that the Yamuna itself, or a channel of the Yamuna, along with a channel of the Sutlej may have flowed west some time between 47,000 BCE and 10,000 BCE, well before the beginnings of Indus civilization. Recent geophysical research shows that during the mature time of the Harappan Civilisation, the Ghaggar-Hakra system became a system of monsoon-fed rivers, after the course change of Sutlej river about 8,000 years ago. [11] Satellite photography has shown that the Ghaggar-Hakra was a large river that dried up several times. [2] The Hakra river is hydraulically connected to the Nara River provided it has adequate flow to maintain surface flow. The Mahabharata says that the Sarasvati River dried up in a desert (at a place named Vinasana or Adarsana).[40]. (2020) state that "most workers have documented the cessation of large scale fluvial activity in NW India in early Holocene, thereby refuting the sustenance of the Harappan civilization by a large river. [4] The Indus Valley Civilisation declined when the monsoons that fed the rivers diminished at around some 4,000 years ago. Hakra or Hakro Darya streamed through Sindh and its sign can be found in Sindh areas such as Khairpur, Nawabshah, Sanghar and Tharparkar. Potential sources for this river include the Yamuna River, the Sutlej River, or both rivers. Along the course of the Ghaggar-Hakra river, there are many early archaeological sites belonging to the Indus Valley Civilization; but not further south than the middle of Bahawalpur district. [4], The basin is classified in two parts, Khadir and Bangar, the higher area that is not flooded in rainy season is called Bangar and the lower flood-prone area is called Khadar.[5]. Some paleo-environmental scientists have proposed that the Hakkra was fed by Himalayan sources, which made it a mighty river,[note 5] but dried-up between 2500 BCE and 1900 BCE, due to tectonic disturbances which caused a tilt in topography of Northwest India, resulting in the migration of rivers. "[17], Mughal, summing up the evidence, concludes that during the Bronze Age the Ghaggar-Hakra sometimes carried more, sometimes less water. [10], The Hakra is the dried-out channel of a river near Fort Abbas City in Pakistan that is the continuation of the Ghaggar River in India. 2B). [13], According to Mugal the Sutlej may have flowed periodically into the Ghaggar-Hakra river bed. The older one described in the family books of the Rigveda, which he calls Naditama Sarasvati, drains into a samudra. It was perennial after the last Ice Age due to reactivation from Satluj, during the pre, early and middle Harappan period, from 7000BCE to 2500BCE. The abandonment of this older course by the Sutlej started 15,000 years ago, and was complete by 8,000 years ago. The Ghaggar is an intermittent river in India, flowing during the monsoon rains. Ghaggar in Haryana. It originates in the village of Dagshai in the Shivalik Hills of Himachal Pradesh at an elevation of 1,927 metres (6,322 ft) above mean sea level[8] and flows through Punjab and Haryana states into Rajasthan;[9] just southwest of Sirsa, Haryana and by the side of Talwara Lake in Rajasthan. The main tributaries of the Ghaggar are the Kaushalya river, Markanda, Sarsuti, Tangri and Chautang. Many early settlements are found along the river beds in this area. Several times, but not continuously, it carried the water of the Sutlej and Ghaggar during the Bronze Age period. Ghaggar hotels map is available on the target page linked above. This place is situated in Multan, Punjab, Pakistan, its geographical coordinates are 30° 26' 0" North, 71° 44' 0" East and its original name (with diacritics) is Ghaggar.

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