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The Ghaggar river flows into the Ottu reservoir, afterwards it becomes the Hakra river Ghaggar river's dry bed in February near Naurangdesar village, Hanumangarh district, Rajasthan, India. Ghaggar river, near Anoopgarh, Rajasthan in the month of September. The Ghaggar is an intermittent river in India, flowing during the monsoon rains.
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 Sirsa, 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 City in Haryana, India. [1]
The Ghaghara River, also known as the Karnali River in Nepal, Mapcha Tsangpo in Tibet, and as the Sarayu River in the lower Ghaghara of India's Awadh, [1] [2] is a perennial trans-boundary river that originates in the northern slopes of the Himalayas in the Tibetan Plateau, cuts through the Himalayas in Nepal and joins the Sharda River at Brahmaghat in India.
Further downstream on the banks of the Ghaggar stands an old derelict fort at Sirsa town named Sarsuti. [4] After the Ottu barrage, the Ghaggar river is called the Hakra River and in Sindh it is called the Nara River. The order of rivers from left to right is the Ghaggar, Dangri, Markanda and Sarsuti.
The Chautang river is a seasonal river in the state of Haryana, India. It is theorized by some to be a remnant of the ancient river Drishadvati. [3] It joins the Ghaggar-Hakra River east of Suratgarh in Rajasthan. [4] According to McIntosh, this river was one of the main contributors to this river system until the Yamuna changed its course. [3]
Ghaggar-Hakra River: An intermittent river in India and Pakistan that flows only during the monsoon season. While it is often identified with the Sarasvati River, [2] this is not a consensus view. [3] The Hakra is the dried-out channel of a river in Pakistan that is the continuation of the Ghaggar River in India. Several times, but not ...
There is substantial geologic evidence to indicate that prior to 1700 BC, and perhaps much earlier, the Sutlej was an important tributary of the Ghaggar-Hakra River (thought to be the legendary Sarasvati River) rather than the Indus, with various authors putting the redirection from 2500 to 2000 BC, [14] from 5000 to 3000 BC, [15] or before ...
Français : Ancien lit de la rivière Ghaggar-Hakra. Le segment en turquoise est le lit récent de la rivière Sutlej vers 9000 av. J-C., en magenta, le lit original de la rivière Ghaggar-Hakra, en indigo le lit du Sutlej lors de l'apogée de la civilisation harappéenne et en rose l'hypothèse d'une rivière Drishadvati alimentant le Ghaggar-Hakra.