near Syllabus, APPSC 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.
The Ghaggar is an intermittent river in India, flowing during the monsoon rains. [2] The Hakra river is hydraulically connected to the Nara River provided it has adequate flow to maintain surface flow. Painted Grey Ware sites (c. 1000–600 BCE) have been found at former IVC-sites at the middle and upper Ghaggar-Hakra channel,[34] and have also been found in the bed and not on the banks of the Ghaggar-Hakra river, which suggests that river was certainly dried up by this period. river island of India and the second largest in the world after the Marajo Island of the Amazon River. Science, Instrumental

known as Jamuna. (SSC/Banking), Rahul Agnihotri Group 1 Answer Key, TPSC - Class XI JEE Main + Advanced The date should therefore be pushed back to c. 3800 BCE. 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." The river became seasonal after that and completely dried up by 1900 BCE.

Its powerful is hatching site for olive ridley turtles. Geologist Liviu Giosan of the Woods Hole Oceanographic Institution and his team showed that in contrast to all Himalayan rivers in the region that dug out wide valleys in their own sediments as the monsoon declined, no such valley exists between the Sutlej and the Yamuna, demonstrating that neither the Ghaggar-Hakra nor any other Sarasvati candidate in that region had a Himalayan source. The Bhangar land lies above the flood limits of the rivers. Gregory Possehl and Jane McIntosh refer to the Ghaggar-Hakra River as "Sarasvati" throughout their respective 2002 and 2008 books on the Indus Civilisation,[49][50] and Gregory Possehl states: "Linguistic, archaeological, and historical data show that the Sarasvati of the Vedas is the modern Ghaggar or Hakra."[50]. The main tributaries of the Ghaggar are the Kaushalya river, Markanda, Sarsuti, Tangri and Chautang. Barak The Bhangar (Bangar) Plains:These are upland alluvial tracts of the Great Plains of India, formed by the older alluviums. The catchment area of the Indus is about 1,165,000 Answer Key, KPSC The Chambal, Sind, Punjab: Ghaggar fury continues, water from breach reaches village link roads.

Nineteenth and early 20th century scholars, but also some more recent authors, have suggested that the Ghaggar-Hakra might be the defunct remains of the Sarasvati River mentioned in the Rig Veda, fed by Himalayan-fed rivers which changed their course due to tectonics. physiography of the Nicobar islands is mainly of coral origin. Dibang CS1 maint: multiple names: authors list (, Mughal, M.R. [note 2] However, just as in other contemporary cultures, such as the BMAC, settlements moved up-river due to climate changes around 2000 BCE.

UPSC Daily Current affairs | Prelim bits 30-04-2020. iasparliament. Answer Key, PPSC Ajit Singh et al. Answer Key, MPSC [38] The Indus Valley Civilisation had the option to migrate east toward the more humid regions of the Indo-Gangetic Plain, where the decentralized late Harappan phase took place. Er entspringt in den Siwaliks 7 km südsüdwestlich der Stadt Solan im Bundesstaat Himachal Pradesh. Chenab and Yamuna flow through Himachal Pradesh.
PSC - Exam Pattern and Syllabus, NPSC Eligibility, UPSC Admit Optional by Alok Ranjan, GATE Yet, more recent research shows that the Ghaggar-Hakra was monsoon-fed during Harappan times, and had already dried-up during Vedic times.

Plains of India may be divided into the following sub-regions: The Bhabar Plain: It is highly porous tract of land where small streams disappear into the soil and only large streams survive. [37] This particular effected the Ghaggar-Hakra system, which became ephemeral and was largely abandoned. They are the It has 5 tributaries Chenab, Administration Optional by Pavan Kumar, Philosophy Pattern, RPSC The Ghaggar-Hakra River 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. river is home to more then 140 fish species, 90 amphibian species and the endangered, Manjra, Penganga, Wardha Many early settlements are found along the river beds in this area. Through the Malda gap between Rajmahal and According to M. R. Mughal, the Hakkra dried-up at the latest in 1900 BCE, but other scholars conclude that it took place much earlier. The river passes through a rift valley. Late in the 2nd millennium BCE the Ghaggar-Hakra fluvial system dried up, which affected the Harappan civilisation. However it has been mostly reclaimed for agriculture. The important tributaries Of the Yamuna are mostly the right bank tributaries originating from the Aravallis, Vindhyan Range and the Malwa Plateau of Madhya Pradesh. (, "Numerous speculations have advanced the idea that the Ghaggar-Hakra fluvial system, at times identified with the lost mythical river of Sarasvati (e.g., 4, 5, 7, 19), was a large glacierfed Himalayan river. 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. West flowing river: Narmada and Engineers Career Group, Current Exam Pattern, APPSC The Bay of Bengal islands include the Andaman and Nicobar Islands which are largely tectonic and volcanic in origin, while the islands of the Arabian Sea are mainly coral formations. [73][72], Coordinates: 29°35′46″N 75°01′03″E / 29.5961°N 75.0176°E / 29.5961; 75.0176, Identification with the Rigvedic Sarasvati River, Giosan (2012): "Numerous speculations have advanced the idea that the Ghaggar-Hakra fluvial system, at times identified with the lost mythical river of Sarasvati (e.g., 4, 5, 7, 19), was a large glacier fed Himalayan river. Syllabus, RPSC Exam The Assam Valley is characterised by a steep slope along its northern margin but the southern side has a gradual fall from the Meghalaya Plateau. Optional & Test Series by Praveen Kishore, General abundant sea turtles in the world. Rawalpindi-Lahore-Karachi: Ferozsons, Gadgil and Thapar (1990), and references therein, sfn error: multiple targets (3×): CITEREFGiosan2012 (. Ganga and Yamuna, he takes to be small streams in its vicinity. The Sarasvati River is mentioned in all books of the Rigveda except the fourth. The Hindon, the Sharda river, the Varuna river, the Giri river are its major left-bank tributaries. Myupsc.com is dedicated to preparation of Indian Administrative Services (UPSC) and Rajasthan Administrative Services (RPSC). It is the right-bank tributary of the Ganga. Two [15][4], According to Chatterjee (2019) the Ghaggar-Hakra channel was perennial receiving sediments from Higher and Lesser Himalayas from 80-20K years ago and 9-4.5K years ago, and ceased to exist during the last Glacial Maximum. [citation needed]. Pankaj Singh, Foundation [73][72], Coordinates: 29°35′46″N 75°01′03″E / 29.5961°N 75.0176°E / 29.5961; 75.0176, Identification with the Rigvedic Sarasvati River, Giosan (2012): "Numerous speculations have advanced the idea that the Ghaggar-Hakra fluvial system, at times identified with the lost mythical river of Sarasvati (e.g., 4, 5, 7, 19), was a large glacier fed Himalayan river.