World Library  
Flag as Inappropriate
Email this Article

West Rapti River

Article Id: WHEBN0027506751
Reproduction Date:

Title: West Rapti River  
Author: World Heritage Encyclopedia
Language: English
Subject: Rohni River, Madi, Kham Magar, Tulsipur State, List of rivers of Nepal
Collection: Hydroelectric Power Stations in Nepal, International Rivers of Asia, Rivers of Nepal, Rivers of Uttar Pradesh
Publisher: World Heritage Encyclopedia
Publication
Date:
 

West Rapti River

Rāptī Nadī
राप्ती नदी
Origin Rapti Zone, Nepal south of border of Rukum District with Rolpa District
Mouth Ghaghara River
Basin countries Nepal, India
Source elevation 3,500 m (11,500 ft)
Mouth elevation 60 m (200 ft)
Avg. discharge 136 m3/s (4,800 cu ft/s) at mouth
Basin area 23,900 km2 (9,200 sq mi)
River system Ganges
Left tributaries Lungri Khola, Jhimruk Khola, Ami River, Rohini River
Right tributaries Arun Khola,

West Rapti drains Rapti Zone in Mid-Western Region, Nepal, then Awadh and Purvanchal regions of Uttar Pradesh state, India before joining the Ghaghara a major left bank tributary of the Ganges known as the Karnali inside Nepal.

The West Rapti is notable for janajati ethnic groups – Kham Magar among its highland sources and then Tharu in Inner Terai Deukhuri Valley, for its irrigation and hydroelectric potential, and for recurrent floods that led to its nickname "Gorakhpur's Sorrow".

Contents

  • Geography 1
  • Sources and Course 2
  • Ancient river 3
  • History 4
  • Development 5
  • References 6

Geography

The Rapti rises south of a prominent E-W ridgeline midway between the western Dhaulagiri Himalaya and the Mahabharat Range. A 3,500 metres (11,500 ft) summit on this ridgeline marks a triple divide. North of the triple divide the Karnali and Gandaki basins are adjacent; south of it the Rapti and similar but smaller Babai River (Nepali: बबई नदी; Babaī Nadī) separate the two larger basins. After crossing into India, the Babai and Rapti separately join the Karnali's continuation called Ghaghara. The Ghaghara ultimately joins the Ganges, as does the Gandaki.

Sources and Course

The Rapti's headwaters descend south from rugged highlands populated by Mahabharat Range.

Jhimruk Kholā (Nepali: झिमरुक खोला) -- east of the Mardi—mainly drains Pyuthan. Below the upper highlands, an alluvial valley opens where Bahun and Chhetri rice farmers irrigate paddy fields. At Cherneta, Pyuthan the Jhimruk approaches within 1.5 km of the Mardi and a 12 megawatt hydroelectric plant exploits the Jhimruk being 200 meters higher.

Below Cherneta the Jhimruk loops east, becoming the border between Pyuthan and Siwalik Hills and Dang District. At Bhalubang Bazaar Nepal's east-west Mahendra Highway bridges the river.

Below Bhalubang, Inner Terai Deukhuri Valley opens between the Dang and Dudhwa Ranges, both subranges of the Siwaliks. Valley, following the WNW trend of the Siwalik hills for 100 km. Although the land is fertile, before DDT came into use in the 1950s Deukhuri was so malarial that only the Tharu people who had genetic resistance could be confident of surviving the warmer months.

The river crosses from Dang into Banke District. Approaching Nepalganj—largest town in Nepal's western Terai—the Dudhwa Hills fall away and the river turns SE, crossing into Uttar Pradesh, India and flowing through districts Shravasti, Siddharth Nagar, Basti, Sant Kabir Nagar and Gorakhpur, passing Gorakhpur city at about 135 air miles (215 km) from Nepal.

Just west of the city it is joined by the smaller Rohini rising further east in Nepal's Nawalparasi and Rupandehi Districts, draining 794 km2 in Nepal then 1892 km2 in India. 60 km beyond Gorakhpur the Rapti joins the Ghaghara (Karnali) at Rajpur. About 120 km further on at Chhapra, the Ghaghara reaches the Ganges.[1][2][3]

[4]

Ancient river

Aciravati, an ancient river has been identified with the modern Rapti.[5] .[6]

History

House of Tulsipur

Development

The Rapti's flow has great seasonal variation because the river lacks sources in high elevation glaciers and snowfields to buffer pre-monsoon drought. Average monthly flows at Jalkundi (27°58'N, 82°14'E) in Deukhuri Valley vary from 17.6 cumecs in pre-monsoon April to 451 cumecs at the peak of the monsoon in August. Maximum recorded flood was 7,390 cumecs on 10 September 1981. 100-year flood flows are predicted at 10,100 cumecs. Over 700,000 acres (280,000 ha) in Uttar Pradesh are at risk of floods every year.

Flood control projects under study include a dam at Jalkundi that would inundate 71,000 acres (29,000 ha) of farmland in Deukhuri Valley. An alternative dam site is upstream at Naumure on the Pyuthan-Dang district border (27°53'N, 82°48'E). This would be an earthen dam 169 m high with 351 million cubic meters live storage capacity, storing excess monsoon flows for irrigation use during the following dry season and generating up to 207 megawatts. Impoundment would mainly be in gorges through the Mahabharat Range, inundating less farmland than the Jalkundi alternative.

Plans are also underway for three irrigation sub-projects – Kapilvastu District 30,500 hectares (75,000 acres) involving interbasin water transfer to the southeast, Deukhuri Valley 9,500 hectares (23,000 acres), and Banke District 40,000 hectares (99,000 acres).[7]

References

  1. ^ "Rapti River". india9. Retrieved 2010-05-28. 
  2. ^ "Basti". Basti district administration. Retrieved 2010-05-30. 
  3. ^ "Sant Kabir Nagar district". Sant Kabir Nagar district administration. Retrieved 2010-05-30. 
  4. ^ Negi, Sharad Sing. "Himalayan rivers, glaciers and lakes". p. 115. Google books. Retrieved 2010-05-28. 
  5. ^ Kapoor, Subodh. "Encyclopaedia of Ancient Indian Geography". p. 5. Google books. Retrieved 2010-08-18. 
  6. ^ Hoey, William. (1907). "The Five Rivers of the Buddhists". Journal of the Royal Asiatic Society of Great Britain and Ireland: 41–46. Retrieved 2011-03-10. 
  7. ^ Dwarika N. Dhungel, Santa B. Pun. "The Nepal-India Water Relationship: Challenges". p. 93, p. 389. Google books. Retrieved 2010-05-28. 
This article was sourced from Creative Commons Attribution-ShareAlike License; additional terms may apply. World Heritage Encyclopedia content is assembled from numerous content providers, Open Access Publishing, and in compliance with The Fair Access to Science and Technology Research Act (FASTR), Wikimedia Foundation, Inc., Public Library of Science, The Encyclopedia of Life, Open Book Publishers (OBP), PubMed, U.S. National Library of Medicine, National Center for Biotechnology Information, U.S. National Library of Medicine, National Institutes of Health (NIH), U.S. Department of Health & Human Services, and USA.gov, which sources content from all federal, state, local, tribal, and territorial government publication portals (.gov, .mil, .edu). Funding for USA.gov and content contributors is made possible from the U.S. Congress, E-Government Act of 2002.
 
Crowd sourced content that is contributed to World Heritage Encyclopedia is peer reviewed and edited by our editorial staff to ensure quality scholarly research articles.
 
By using this site, you agree to the Terms of Use and Privacy Policy. World Heritage Encyclopedia™ is a registered trademark of the World Public Library Association, a non-profit organization.
 



Copyright © World Library Foundation. All rights reserved. eBooks from World eBook Library are sponsored by the World Library Foundation,
a 501c(4) Member's Support Non-Profit Organization, and is NOT affiliated with any governmental agency or department.