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| name = Gandaki River
| name = Gandaki River
| native_name =  
| native_name =  
| native_name_lang   =  
| native_name_lang =  
| name_other = Narayani
| name_other = Narayani
| name_etymology =  
| name_etymology = <!---------------------- IMAGE & MAP -->
<!---------------------- IMAGE & MAP -->
| image = {{Photomontage
| image = {{Photomontage
| photo1a = Narayani bridge in Gaindakot.jpg
| photo1a = Narayani bridge in Gaindakot.jpg
| photo2a = Sonepur- gandak bridge -Hajipur (5448565068).jpg
| photo2a = Sonepur- gandak bridge -Hajipur (5448565068).jpg
|photo3a =narayani.jpg
| photo3a = Valmiki Nagar Barrage on the Gandaki River at the Indo–Nepal border between West Champaran District in Bihar (India) and Nawalparasi District in Nepal.01.jpg
| spacing = 3
| spacing = 3
| color_border = white
| color_border = white
| color =  
| color =  
| image_size = 285
| image_size =
}}
}}
| image_caption     = '''From top''': Narayani River in [[Chitwan]],<br />Gandak River in [[Hajipur]]<br />Gandak River in [[Nepal]]
| image_caption = '''From top''': Narayani River in [[Chitwan]], Gandak River in [[Hajipur]], Gandak River in [[Nepal]], The Gandak River Barrage in [[West Champaran]] [[Bihar]].
Anoma River in [[Buddhist Era]]
| map = River Ganges and tributaries.png
| map = River Ganges and tributaries.png
| map_size =  
| map_width =  
| map_caption = Map showing the [[Ghaghara]] and Gandaki tributaries of the [[Ganges]]
| map_caption = Map showing the [[Ghaghara]] and Gandaki tributaries of the [[Ganges]]
| pushpin_map =  
| pushpin_map =  
| pushpin_map_size =  
| pushpin_map_size =  
| pushpin_map_caption=  
| pushpin_map_caption = <!---------------------- LOCATION -->
<!---------------------- LOCATION -->
| subdivision_type1 = Country
| subdivision_type1 = Country
| subdivision_name1 = [[Nepal]], [[India]]
| subdivision_name1 = [[Nepal]], [[India]]
| subdivision_type2 =  
| subdivision_type2 =  
| subdivision_name2 =  
| subdivision_name2 =  
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| subdivision_name4 =  
| subdivision_name4 =  
| subdivision_type5 = Cities
| subdivision_type5 = Cities
| subdivision_name5 = [[Lo Manthang]], [[Jomsom]], [[Beni, Dhawalagiri|Beni]], [[Kusma, Nepal|Kusma]], [[Pokhara]], [[Gorkha Municipality|Gorkha]], [[Ridi]], [[Devghat]], [[Narayangarh, Chitwan|Narayangarh]], [[Valmikinagar]], [[Triveni, Nepal]], [[Hajipur]], [[Sonpur, Nepal|Sonpur]], [[Bagaha]]
| subdivision_name5 = [[Lo Manthang]], [[Jomsom]], [[Beni, Dhawalagiri|Beni]], [[Baglung]], [[Kusma, Nepal|Kusma]], [[Pokhara]], [[Gorkha Municipality|Gorkha]], [[Ridi]], [[Devghat]], [[Narayangarh, Chitwan|Narayangarh]], [[Valmikinagar]], [[Triveni, Nepal]], [[Hajipur]], [[Sonpur, Nepal|Sonpur]], [[Muzaffarpur]], [[Bagaha]]
<!---------------------- PHYSICAL CHARACTERISTICS -->
<!---------------------- PHYSICAL CHARACTERISTICS -->
| length = {{convert|814|km|mi|abbr=on}}  
| length = {{cvt|814|km}}
| width_min =  
| width_min =  
| width_avg =  
| width_avg =  
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| depth_max =  
| depth_max =  
| discharge1_location =  
| discharge1_location =  
| discharge1_min = {{convert|500|m3/s|cuft/s|abbr=on}}
| discharge1_min = {{cvt|500|m3/s|cuft/s}}
| discharge1_avg = {{convert|2025|m3/s|cuft/s|abbr=on}}
| discharge1_avg = {{cvt|2025|m3/s|cuft/s}}
| discharge1_max= {{convert|30000|m3/s|cuft/s|abbr=on}}
| discharge1_max = {{cvt|30000|m3/s|cuft/s}}
<!---------------------- BASIN FEATURES -->
<!---------------------- BASIN FEATURES -->
| source1 = Nhubine Himal Glacier
| source1 = Nhubine Himal Glacier
| source1_location = [[Mustang District]], Nepal
| source1_location = [[Mustang District]], Nepal
| source1_coordinates= {{coord|29|17|0|N|85|50|5|E|type:river_region:IN|display=inline}}
| source1_coordinates = {{coord|29|17|19|N|83|52|39|E|type:river_region:IN|display=inline}}
| source1_elevation = {{convert|6268|m|abbr=on}}
| source1_elevation = {{cvt|6268|m}}
| mouth = [[Ganges]]
| mouth = [[Ganges]]
| mouth_location = Sonpur, India
| mouth_location = Sonpur, India
| mouth_coordinates = {{coord|25|39|9|N|85|11|4|E|type:river_region:IN|display=inline,title}}
| mouth_coordinates = {{coord|25|39|9|N|85|11|4|E|type:river_region:IN|display=inline,title}}
| mouth_elevation   = {{convert|44|m|abbr=on}}
| mouth_elevation = {{cvt|44|m}}
| progression =  
| progression =  
| river_system =  
| river_system =  
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| tributaries_left = [[Trishuli River|Trishuli]]
| tributaries_left = [[Trishuli River|Trishuli]]
| tributaries_right = [[Kali Gandaki]]
| tributaries_right = [[Kali Gandaki]]
| custom_label =
| custom_label =  
| custom_data =  
| custom_data =  
| extra =  
| extra =
}}
}}


The '''Gandaki River''', also known as the '''Narayani''' and the '''Gandak''', is one of the major rivers in Nepal and a [[:wikt:left bank|left bank]] tributary of the [[Ganges]] in India. Its total catchment area amounts to {{cvt|46300|km2|sqmi|sp=us}}, most of it in Nepal. In the Nepal [[Himalayas]], it is notable for its deep [[canyon]]. The basin also contains three mountains over {{cvt|8000|m}}, namely [[Dhaulagiri]], [[Manaslu]] and [[Annapurna Massif|Annapurna]] I. Dhaulagiri is the highest point of the Gandaki basin.
The '''Gandaki River''', also known as the '''Narayani''' and '''Gandak''', is one of the major rivers in [[Nepal]] and a left-bank tributary of the [[Ganges]] in [[India]]. Its total catchment area is {{cvt|46300|km2|sqmi|sp=us}}, most of it in Nepal. In the Nepal [[Himalayas]], the Gandaki is notable for its deep [[canyon]]. The basin also contains three mountains over {{cvt|8000|m}}, namely [[Dhaulagiri]], [[Manaslu]] and [[Annapurna Massif]]. Dhaulagiri is the highest point of the Gandaki basin. In its upper reaches, the river is known as '''Kali Gandaki''' (or Gandaki) as it flows through the [[Mustang District]] and the famous [[Kali Gandaki Gorge]] in Nepal.  When the river reaches the Terai plains of Nepal, it is referred to as the '''Narayani''' River. This name change typically occurs near the confluence with the [[Trishuli River]] at [[Devghat]] in [[Chitwan]]. Upon entering India, the river is known as the '''Gandak''' River.


==River course==
==River course==
===Nepal===
===Nepal===
[[File:Panorama of the Kali Gandaki gorge in Upper Mustang.jpg|thumb|Panorama of the Kali Gandaki gorge in Upper Mustang]]
[[File:Panorama of the Kali Gandaki gorge in Upper Mustang.jpg|thumb|Panorama of the Kali Gandaki gorge in Upper Mustang]]
[[File:Kali Gandaki river north of Kagbeni.jpg|thumb|Kali Gandaki river north of Kagbeni]]
[[File:1 River Gandhak Gandaki in Kagbeni Nepal before entering India.jpg|thumb|River Gandaki in Kagbeni, Nepal]]
[[File:GandakiKagbeni.JPG|thumb|In Nepal, the river quickly crosses different climate zones]]
[[File:GandakiPineForest.JPG|thumb|Gandaki River flows through a pine forest {{convert|25|km|mi|abbr=on}} downstream from the place above]]


The Kali Gandaki [[river source]] is at the border with [[Tibet]] at an elevation of {{convert|6268|m|ft}} at the Nhubine Himal Glacier in the [[Mustang (kingdom)|Mustang]] region of Nepal.<ref>{{cite map |title= Upper& Lower Mustang |scale= 1:70000 |publisher= Nepal Map Publisher Pvt., Ltd. |location=Kathmandu}}</ref><ref>{{Cite journal |last=Garzione |first=C. N. |name-list-style=amp |author2=Quade, J. |author3=DeCelles, P.G. |author4=English, N.B. |title=Predicting paleoelevation of Tibet and the Himalaya from δ18O vs. altitude gradients in meteoric water across the Nepal Himalaya |journal=Earth and Planetary Science Letters |volume=183 |issue=1–2 |pages=215–229 |year=2000 |bibcode=2000E&PSL.183..215G |doi=10.1016/S0012-821X(00)00252-1 |author-link=Carmala Garzione}}</ref>
The Kali Gandaki [[river source]] is at the border with [[Tibet]] at an elevation of {{cvt|6268|m}} at the Nhubine Himal Glacier in the [[Mustang (kingdom)|Mustang]] region of Nepal.<ref>{{cite map |title= Upper& Lower Mustang |scale= 1:70000 |publisher= Nepal Map Publisher Pvt., Ltd. |location=Kathmandu}}</ref><ref>{{Cite journal |last=Garzione |first=C. N. |name-list-style=amp |author2=Quade, J. |author3=DeCelles, P.G. |author4=English, N.B. |title=Predicting paleoelevation of Tibet and the Himalaya from δ18O vs. altitude gradients in meteoric water across the Nepal Himalaya |journal=Earth and Planetary Science Letters |volume=183 |issue=1–2 |pages=215–229 |year=2000 |bibcode=2000E&PSL.183..215G |doi=10.1016/S0012-821X(00)00252-1 |author-link=Carmala Garzione}}</ref>


{{Unreferenced section|date=January 2021}}
{{Unreferenced section|date=January 2021}}
The headwaters stream on some maps is named the Chhuama Khola and then, nearing [[Lo Manthang]], the Nhichung Khola or Choro Khola. The Kali Gandaki then flows southwest (with the name of '''Mustang Khola''' on old, outdated maps) through a sheer-sided, deep canyon before widening at the steel footbridge at Chele, where part of its flow funnels through a rock tunnel, and from this point the now wide river is called the Kali Gandaki on all maps. In [[Kagbeni, Mustang|Kagbeni]] a major tributary named Johng Khola, Kak Khola or Krishnaa descends from [[Muktinath]].
The headwater stream on some maps is named the Chhuama Khola and then, nearing [[Lo Manthang]], the Nhichung Khola or Choro Khola. The Kali Gandaki then flows southwest (with the name of '''Mustang Khola''' on old, outdated maps) through a sheer-sided, deep canyon before widening at the steel footbridge at Chele, where part of its flow funnels through a rock tunnel, and from this point the now wide river is called the Kali Gandaki on all maps. In [[Kagbeni, Mustang|Kagbeni]] a major tributary named Johng Khola, Kak Khola or Krishnaa descends from [[Muktinath]].


The river then flows southward through a steep gorge known as the '''[[Kali Gandaki Gorge]]''', or '''Andha Galchi''', between the mountains [[Dhaulagiri]], elevation {{convert|8167|m|ft}} to the west and [[Annapurna|Annapurna I]], elevation {{convert|8091|m|ft}} to the east. If one measures the depth of a canyon by the difference between the river height and the heights of the highest peaks on either side, this gorge is the world's deepest. The portion of the river directly between Dhaulagiri and Annapurna I, {{convert|7|km|mi|0}} downstream from [[Tukuche]]), is at an elevation of {{convert|2520|m|ft}},<ref name="anna_map">''Annapurna'' (1:100,000 map), Nepal-Kartenwerk der Arbeitgemeinschaft für vergleichende Hochgebirgsforschung Nr. 9, Nelles Verlag, Munich, 1993. Also see [http://earth.google.com Google Earth]</ref> which is {{convert|5571|m|ft}} lower than Annapurna I.  The river is older than the Himalayas.  As tectonic activity forces the mountains higher, the river has cut through the uplift.
The river then flows southward through a steep gorge known as the '''[[Kali Gandaki Gorge]]''', or '''Andha Galchi''', between the mountains [[Dhaulagiri]], elevation {{cvt|8167|m}} to the west and [[Annapurna]], elevation {{cvt|8091|m}} to the east. If one measures the depth of a canyon by the difference between the river height and the heights of the highest peaks on either side, this gorge is the world's second deepest after the [[Yarlung Tsangpo Grand Canyon]] (ca. 6000 m). The portion of the river directly between Dhaulagiri and Annapurna I, {{cvt|7|km}} downstream from [[Tukuche]]), is at an elevation of {{cvt|2520|m}}, which is {{cvt|5571|m}} lower than Annapurna I.  The river is older than the Himalayas.  As tectonic activity forces the mountains higher, the river has cut through the uplift.
South of the gorge, the river is joined by [[Rahughat Khola]] at Galeshwor, Myagdi Khola at [[Beni, Dhawalagiri|Beni]], Modi Khola near [[Kushma]] and Badigaad at Rudrabeni above Ridi Bazaar. The river then turns east to run along the northern edge of the [[Mahabharat Range]]. One of the largest [[hydroelectricity]] project in Nepal is located along this stretch of the river. Turning south again and breaking through the Mahabharats, Kali Gandaki is then joined by a major tributary, the [[Trishuli River|Trishuli]], at [[Devghat]], which is larger than the Kali Gandaki. Gandaki is then joined by the [[East Rapti River]] draining the [[Inner Terai Valleys of Nepal|Inner Terai valley]] known as [[Chitwan Valley|Chitwan]].  The Gandaki then crosses the outermost foothills of the Himalayas—[[Sivalik Hills]]—into the Terai plains of Nepal. From Devghat, the river flows southwest of [[Gaindakot]] town. The river later curves back towards the southeast as it enters India where it is called the Gandak.
South of the gorge, the river is joined by [[Rahughat Khola]] at Galeshwor, Myagdi Khola at [[Beni, Dhawalagiri|Beni]], Modi Khola near [[Kushma]] and Badigaad at Rudrabeni above Ridi Bazaar. The river then turns east to run along the northern edge of the [[Mahabharat Range]]. One of the largest [[hydroelectricity]] project in Nepal is located along this stretch of the river. Turning south again and breaking through the Mahabharats, Kali Gandaki is then joined by a major tributary, the [[Trishuli River|Trishuli]], at [[Devghat]], which is larger than the Kali Gandaki. Gandaki is then joined by the [[East Rapti River]] draining the [[Inner Terai Valleys of Nepal|Inner Terai valley]] known as [[Chitwan Valley|Chitwan]].  The Gandaki then crosses the [[Sivalik Hills]] into the Terai plains of Nepal. From Devghat, the river flows southwest of [[Gaindakot]] town. The river later curves back towards the southeast as it enters India where it is called the Gandak.


Below Gaindakot the river is known as the '''Narayani''' or '''Sapt Gandaki''' (Seven Gandakis), for seven tributaries rising in the Himalaya or further north along the main [[Ganges River|Ganges]]-[[Brahmaputra River|Brahmaputra]] divide.  These are the Kali Gandaki, the Trishuli River, and the five main tributaries of the Trishuli known as the Daraudi, [[Seti Gandaki River|Seti]], Madi, [[Marsyandi]] and [[Budhi Gandaki River|Budhi Gandaki]].
Below Gaindakot the river is known as the '''Narayani''' or '''Sapt Gandaki''' (Seven Gandakis), for seven tributaries rising in the Himalaya or further north along the main [[Ganges River|Ganges]]-[[Brahmaputra River|Brahmaputra]] divide.  These are the Kali Gandaki, the Trishuli River, and the five main tributaries of the Trishuli known as the Daraudi, [[Seti Gandaki River|Seti]], Madi, [[Marsyandi]] and [[Budhi Gandaki River|Budhi Gandaki]].
[[File:1 River Gandhak Gandaki in Kagbeni Nepal before entering India.jpg|left|thumb|River Gandaki in Kagbeni Nepal]]


===India===
===India===
The entry point of the river at the Indo–Nepal border is also the confluence called Triveni with rivers Pachnad and Sonha descending from Nepal. Pandai river flows into Bihar (India) from Nepal in the eastern end of the Valmiki Sanctuary and meets Masan. The Gandak enters India at first in [[Maharajganj District]] of [[Uttar Pradesh]] for around 25 KM, it also passes through [[Kushinagar District]] before entering Bihar. The Gandak flows southeast {{convert|300|km|mi}} across the [[Gangetic plain]] of [[Bihar]] state through [[West Champaran]], [[Gopalganj district, India|Gopalganj]], [[Saran district|Saran]] and [[Muzaffarpur]] districts. It joins the [[Ganges]] near [[Patna]] just downstream of [[Hajipur]] at [[Sonpur, Bihar|Sonpur]] (also known as Harihar Kshetra). Its drainage area in India is {{convert|7620|km2|mi2}}.
The entry point of the river at the Indo–Nepal border is also the confluence called Triveni with the rivers [[Pachnad]] and [[Sonha (river)|Sonha]] descending from [[Nepal]]. [[Pandai]] river flows into [[Bihar]] from [[Nepal]] in the eastern end of the [[Valmiki Sanctuary]] and meets Masan. The [[Gandak]] enters [[India]] at first in [[Maharajganj District]] of [[Uttar Pradesh]] for around {{cvt|25|km}}; it also passes through [[Kushinagar District]] before entering [[Bihar]]. The [[Gandak]] flows southeast {{cvt|300|km}} across the [[Gangetic plain]] of [[Bihar]] state through [[West Champaran]], [[Gopalganj district, India|Gopalganj]], [[East Champaran district|East Champaran]], [[Saran district|Saran]], [[Muzaffarpur]] and [[Vaishali district|Vaishali]] districts.<ref>{{Cite web |title=River Basin|url=https://www.fmiscwrdbihar.gov.in/fmis/Riverbasin.html |access-date=2024-03-07 |work=Flood Management Improvement Support Centre, Water Resources Department of Government of Bihar}}</ref>


From its exit from the outermost [[Siwaliks]] foothills to the Ganges, the Gandak has built an immense [[alluvial fan|megafan]] comprising Eastern Uttar Pradesh and North Western Bihar in the Middle Gangetic Plains.<ref>{{cite web |url=http://www.industcards.com/hydro-india.htm |archive-url=https://archive.today/20120904145551/http://www.industcards.com/hydro-india.htm |url-status=dead |archive-date=4 September 2012 |title=hydro-india-other |publisher=Industcards.com |access-date=28 November 2009 }}</ref> The megafan consists of sediments eroded from the rapidly uplifting Himalaya. The river's course over this structure is constantly shifting.
From its exit from the outermost [[Siwaliks]] foothills to the [[Ganga]], the [[Gandak]] has built an immense [[alluvial fan|megafan]] comprising Eastern [[Uttar Pradesh]] and North Western [[Bihar]] in the Middle [[Gangetic Plains]].<ref>{{cite web |url=http://www.industcards.com/hydro-india.htm |archive-url=https://archive.today/20120904145551/http://www.industcards.com/hydro-india.htm |url-status=usurped |archive-date=4 September 2012 |title=hydro-india-other |work=Industcards.com |access-date=28 November 2009}}</ref>


==Glaciers, glacial lakes and glacial lake outburst floods==
==Glaciers, glacial lakes and glacial lake outburst floods==
The Gandaki river basin is reported to contain 1025 glaciers and 338 lakes.{{citation needed|date=June 2022}} These contribute substantially to the lean season flows of the river.
Glacier lakes, among the most hazardous features of high mountains, are usually formed behind dams of moraine debris left behind by retreating glaciers, a trend that is observed all over the world. Even though [[glacial lake outburst flood]] (GLOF) events have been occurring in Nepal for many decades, the Dig Tsho glacier outburst, which took place in 1985, has triggered detailed study of this phenomenon. In 1996, the Water and Energy Commission Secretariat (WECS) of Nepal reported that five lakes were potentially dangerous, namely, Dig Tsho, [[Imja Tsho, Nepal|Imja]], Lower Barun, [[Tsho Rolpa]], and Thulagi, all lying above {{cvt|4100|m}}. A recent study done by ICIMOD and UNEP (UNEP, 2001) reported 27 potentially dangerous lakes in Nepal. In ten of them GLOF events have occurred in the past few years and some have been regenerating after the event.{{cn|date=November 2024}}


Glacier lakes, among the most hazardous features of high mountains, are usually formed behind dams of moraine debris left behind by retreating glaciers, a trend that is observed all over the world. Even though [[glacial lake outburst flood]] (GLOF) events have been occurring in Nepal for many decades, the Dig Tsho glacier outburst, which took place in 1985, has triggered detailed study of this phenomenon. In 1996, the Water and Energy Commission Secretariat (WECS) of Nepal reported that five lakes were potentially dangerous, namely, Dig Tsho, [[Imja Tsho, Nepal|Imja]], Lower Barun, [[Tsho Rolpa]], and Thulagi, all lying above {{convert|4100|m|ft}}. A recent study done by ICIMOD and UNEP (UNEP, 2001) reported 27 potentially dangerous lakes in Nepal. In ten of them GLOF events have occurred in the past few years and some have been regenerating after the event.
The [[Thulagi glacier]], located in the Upper Marsyangdi River basin, is one out of the two moraine-dammed lakes that was identified as a potentially dangerous lake as it may outburst.<ref>{{cite web |url=http://www.bgr.de/lebgeo/thulagi.htm |title=BGR/NLfB/GGA: Gletschersee Thulagi |publisher=Bgr.de |access-date=28 November 2009 |url-status=dead |archive-url=https://web.archive.org/web/20110718202501/http://www.bgr.de/lebgeo/thulagi.htm |archive-date=18 July 2011}}</ref>
 
=== Thulagi glacier ===
The [[Thulagi glacier]], which is located in the Upper Marsyangdi River basin, is one out of the two moraine-dammed lakes (supra-glacial lakes), identified as a potentially dangerous lake. The [[Kreditanstalt für Wiederaufbau|KfW]], [[Frankfurt am Main|Frankfurt]], the BGR (Federal Institute for Geosciences and Natural Resources, Germany), in cooperation with the Department of Hydrology and Meteorology in Kathmandu, have carried out studies on the Thulagi Glacier and have concluded that even assuming the worst case, a disastrous outburst of the lake can be excluded in the near future.<ref>{{cite web |url=http://www.bgr.de/lebgeo/thulagi.htm |title=BGR/NLfB/GGA: Gletschersee Thulagi |publisher=Bgr.de |access-date=28 November 2009 |url-status=dead |archive-url=https://web.archive.org/web/20110718202501/http://www.bgr.de/lebgeo/thulagi.htm |archive-date=18 July 2011 }}</ref>


== Important towns ==
== Important towns ==
[[File:Kaligandaki ghasa.jpg|thumb|Kali Gandaki River near Ghasa, between [[Annapurna]] and [[Dhaulagiri]]]]
[[File:Kaligandaki ghasa.jpg|thumb|Kali Gandaki River near Ghasa, between [[Annapurna]] and [[Dhaulagiri]]]]
The important towns in the Indian part of the Gandak river are Valmikinagar (Bhainsalotan) - location of Gandak Barrage, [[Bagaha]], [[Bettiah]] (district headquarters & field directorate of Valmiki Tiger Project), Harinagar (Ramnagar), [[Hajipur]] (across the Ganges 10&nbsp; km from Patna) and Sonepur (also Known as Harihar Kshetra), near Patna.{{citation needed|date=December 2020}}
The important towns in the Indian part of the Gandak river are Valmikinagar (Bhainsalotan) - location of Gandak Barrage, [[Bagaha]], [[Bettiah]] (district headquarters & field directorate of Valmiki Tiger Project), Harinagar (Ramnagar), [[Hajipur]] (across the Ganges 10&nbsp; km from Patna) and Sonepur (also Known as Harihar Kshetra), near Patna.{{citation needed|date=December 2020}}
==In traditional and popular culture==
[[File:Kali River in Ramghat.jpg|thumb|Gandaki river that divides [[Syangja District]] and [[Palpa District]] in Ramghat]]
{{Unreferenced section|date=January 2021}}
The Gandaki river is mentioned in the ancient [[Sanskrit]] epic [[Mahabharata]].{{citation needed|date=June 2022}}
Its evolution is described in Shiva Purana, Kumarakhand, in the chapter of the killing of Shankhachuda.
Episode 1 of "[[The Living Planet]]," [[David Attenborough]]'s second nature documentary series, is set in the [[Kali Gandaki Gorge]].{{citation needed|date=June 2022}}


== National Parks ==
== National Parks ==
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=== Chitwan National Park ===
=== Chitwan National Park ===
{{Infobox protected area  
{{Infobox protected area
| name = Chitwan National Park
| name = Chitwan National Park
| iucn_category = II
| iucn_category = II
| photo = Rhinos_leofleck.jpg
| image = Rhinos_leofleck.jpg
| photo_caption = Elephant safari after [[Indian rhinoceros]]
| image_caption = Tourists on elephants observing [[Indian rhinoceros]]
}}
}}


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=== Valmiki National Park ===
=== Valmiki National Park ===
Valmiki Sanctuary covers about {{convert|800|km2|mi2}} of forest and was the 18th tiger reserve established in India.<ref>{{cite news|title=Valmiki National Park|work=The Hindu|url=http://www.thehindu.com/todays-paper/tp-features/tp-metroplus/article2244909.ece|date=7 May 2007|access-date=25 October 2014|url-status=live|archive-url=https://web.archive.org/web/20160112234308/http://www.thehindu.com/todays-paper/tp-features/tp-metroplus/article2244909.ece|archive-date=12 January 2016}}</ref> It is ranked fourth in terms density of tiger population. Valmikinagar is located nearly {{convert|100|km|mi}} from Bettiah in the northernmost part of the [[West Champaran district]], Bihar, bordering Nepal. Valmikinagar is a small town with scattered habitation, mostly within the forest area and has a railroad station in the district of West Champaran, close to the railhead of [[Narkatiaganj Junction railway station|Narkatiaganj]]. It has diverse landscapes, sheltering rich wildlife habitats and floral and faunal composition with the prime protected carnivores and was included in the National Conservation Programme of the Project Tiger in the year 1994. As per [[Zoological Survey of India]]'s report of 1998 the sanctuary is reported to shelter 53 mammals, 145 birds, 26 reptile and 13 amphibians.<ref>{{cite web|url=http://discoverbihar.bih.nic.in/pages/wildlife.htm |title=Wildlife Sanctuaries |access-date=3 December 2007 |url-status=dead |archive-url=https://web.archive.org/web/20090410061556/http://discoverbihar.bih.nic.in/pages/wildlife.htm |archive-date=10 April 2009 }}</ref> and Tiger Reserve<ref>{{cite web |url=http://forest.bih.nic.in/ValmikiSanctuary.htm |title=Valmiki Sanctuary |publisher=Forest.bih.nic.in |access-date=28 November 2009 |url-status=dead |archive-url=https://web.archive.org/web/20090915182725/http://forest.bih.nic.in/ValmikiSanctuary.htm |archive-date=15 September 2009 }}</ref>
Valmiki Sanctuary covers about {{convert|800|km2|mi2}} of forest and was the 18th tiger reserve established in India.<ref>{{cite news|title=Valmiki National Park|work=The Hindu|url=http://www.thehindu.com/todays-paper/tp-features/tp-metroplus/article2244909.ece|date=7 May 2007|access-date=25 October 2014|url-status=live|archive-url=https://web.archive.org/web/20160112234308/http://www.thehindu.com/todays-paper/tp-features/tp-metroplus/article2244909.ece|archive-date=12 January 2016}}</ref> It is ranked fourth in terms density of tiger population. Valmikinagar is located nearly {{convert|100|km|mi}} from Bettiah in the northernmost part of the [[West Champaran district]], Bihar, bordering Nepal. Valmikinagar is a small town with scattered habitation, mostly within the forest area and has a railroad station in the district of West Champaran, close to the railhead of [[Bagaha]]. It has diverse landscapes, sheltering rich wildlife habitats and floral and faunal composition with the prime protected carnivores and was included in the National Conservation Programme of the Project Tiger in the year 1994. According to a 1998 report by the [[Zoological Survey of India]], the sanctuary has 53 mammals, 145 birds, 26 reptile and 13 amphibians<ref>{{cite web|url=http://discoverbihar.bih.nic.in/pages/wildlife.htm |title=Wildlife Sanctuaries |access-date=3 December 2007 |url-status=dead |archive-url=https://web.archive.org/web/20090410061556/http://discoverbihar.bih.nic.in/pages/wildlife.htm |archive-date=10 April 2009 }}</ref> and a Tiger Reserve.<ref>{{cite web |url=http://forest.bih.nic.in/ValmikiSanctuary.htm |title=Valmiki Sanctuary |publisher=Forest.bih.nic.in |access-date=28 November 2009 |url-status=dead |archive-url=https://web.archive.org/web/20090915182725/http://forest.bih.nic.in/ValmikiSanctuary.htm |archive-date=15 September 2009 }}</ref>


The notable species of wild fauna include: tiger, leopard, wild dog, wild boar, bison, bear, peacock, partridge, hornbill, [[Gracula|hill mynah]], woolly-necked stork, python, crocodile, deer, [[Sambar deer|sambar]], blue bull, barking deer, hog deer.
The notable species of wild fauna include: tiger, leopard, wild dog, wild boar, bison, bear, peacock, partridge, hornbill, [[Gracula|hill mynah]], woolly-necked stork, python, crocodile, deer, [[Sambar deer|sambar]], blue bull, barking deer, hog deer.
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== Religious significance ==
== Religious significance ==
{{Unreferenced section|date=June 2022}}
[[File:mukthinathsaligram.JPG|thumb|Muktinath Vaishnava temple idols, Nepal]]
 
Between the [[Dhaulagiri]] and [[Annapurna]] mountain ranges, the Gandaki River flows through the village of [[Muktinath]] and by the Ashram of Pulaha. In ancient times, the mountain range surrounding Pulaha was called Salagiris due to the vast forests of [[Shorea robusta|sal]] trees. The stones found in this region are therefore called Saligrama – Silas. It has great significance to Hindus, particularly to Brahmins. Smarthas uses this as the replica of lord Narayana. Srivaisnavas, and [[Madhvacharya]] sects who consider the place where one can find saligrama silas in the river bed of the Gandaki River, and the Mukthinath temple as one of the 108 Divyakshetrams.<ref>{{cite web |url=http://www.sandadesandadi.com/108divyakshetrams.html |title=108divyakshetrams |access-date=30 November 2007 |url-status=dead |archive-url=https://web.archive.org/web/20071224203026/http://www.sandadesandadi.com/108divyakshetrams.html |archive-date=24 December 2007}}</ref>
=== Valmiki Ashram ===
 
The ancient [[Valmiki]]  Ashram (hermitage) and surrounding temples are located in the [[Chitwan National Park]] of Nepal. It is located at a distance of about 7&nbsp;km from [[Valmikinagar]]. It is approachable for pilgrimage only from Valmikinagar near Gandak Barrage, both from Nepal and India.
 
It is said that Valmiki Rishi (sage) wrote the great epic, "[[Ramayana]]" here. It is also believed to be the birthplace of [[Lava (Ramayana)|Lava]] & [[Kusha (Ramayana)|Kusha]] (the two sons of Lord [[Rama|Ram]] and his divine wife [[Sita]]. The hermitage also has landmarks of [[Sita]]'s 'Falahar' (eating place),  Meditation place of the great Sage Valmiki, the place where the [[Ashvamedha|Ashwamedh]] horse was tied, Amrit (nectar of immortality) Kuan (well); [[Vishnu]] Chakra (disc), and the Hawan ([[Yagna]]) [[Kund]] (sacred square structure to perform fire rituals).
 
In the periphery of {{convert|3|to|4|km}} around the Valmiki Ashram, the temples of importance are a) the Jatashankar ([[Shiva|Shiv]]) Temple, 2) Nardevi (Sweta [[Kali]]) Temple (Form of [[Durga]] and 3) Kaleshwaran (an avatar of the God Shiva) Temple. Triveni Temple is located across the Gandak Barrage in Nepal, about 3&nbsp;km from the Gandak Barrage.
 
=== Shaligrams and Mukthinath ===
[[Ammonite]] fossils collected from the bed of the Gandaki River at a place close to Saligrama or [[Muktinath]] (literally "place of salvation") in the Mustang district of Nepal are known as ''[[shaligram]]s'' or ''shilas'' and are considered [[aniconism|aniconic]] representations of [[Vishnu]]. These are first mentioned in "Devi Bhagavath". In the [[puranas]] there is a description of a king, named Dharmadwaja, who was initially a devotee of goddess [[Lakshmi]] and who later became her rival which completely ruined him. His son Padmadwaja realized his father's mistake and became a devotee of Lakshmi. Pleased with his devotion, Lakshmi herself incarnated as [[Tulsi in Hinduism|Tulasi]].
 
Later Tulasi fell in love with Lord Krishna. They married to immortalize their bond. Lord Krishna converted himself as Salagrava (saligram) and Tulasi as the river Gandaki. Even today Salagrava can only be found in the Gandaki river.
 
The Great Master Sri Shankaracharya who knew this story told it to his disciples; that whenever these stones are taken for the purpose of worship one should never worship those shila without Tulasi, to maintain the relation of Tulasi and Sri Krishna. He further said that the Tulasi which we use for worship, is the hair of Tulasi who converted into river Gandaki. Shankaracharya is quoted in his Brahmasutras about the Salagrava: [[yatha salagrame Harihe]], "salagrama eva visno etyethdupayukameva", "yatha slagrame visnuhu sanihita eti tatvat". Even today all his amnaya peetas have a salagrava for their compulsory daily rituals. Silas are considered unique and are used for worship.
 
It is a sacred place for [[Buddhists]] who call it [[Chumig Gyatsa]], which in [[Standard Tibetan|Tibetan]] means 'Hundred Waters'. [[Hindus]] call this place [[Muktinath]] as well as ''Mukthiksehtra'', which literally means "place of salvation".
 
These stones are naturally formed round stones, with circular or spiral markings and are fossil ammonite stones found in the rivers of the [[Himalayas]], in particular kinds of ocean sediments, which have been uplifted to the top of the Himalayas.
 
Between the [[Dhaulagiri]] and [[Annapurna]] mountain ranges, the Gandaki River flows through the village of Saligrama or Muktinath and the Ashrama of Pulaha. In ancient times, the mountain range surrounding Pulaha was called Salagiris due to the vast forests of sala (sal) trees. The stones found in this region are therefore called Saligrama – Silas (stones found only in the region of Saligrama). It has great significance to Hindus, particularly to Brahmins. Smarthas uses this as the replica of lord Narayana. Srivaisnavas, and [[Madhvacharya|Madhva]] sects who consider the place where one can find saligrama silas in the river bed of the Gandaki River, and the Mukthinath temple as one of the 108 Divyakshetrams<ref>{{cite web |url=http://www.sandadesandadi.com/108divyakshetrams.html |title=108divyakshetrams |access-date=30 November 2007 |url-status=dead |archive-url=https://web.archive.org/web/20071224203026/http://www.sandadesandadi.com/108divyakshetrams.html |archive-date=24 December 2007 }}</ref> or Thirthastanas (temples of [[Vishnu]]) to be visited on a pilgrimage (at least once in their life). At the pilgrimage site of Muktinath (3,710m) one wonders in amazement at the presence of 108 small waterfalls and mysterious natural gas fires, worshiped as Jwalamukhi (in Sanskrit).
[[File:mukthinathsaligram.JPG|thumb|right|200px|Muktinath Vaishnava temple idols, Nepal]]
 
For Tibetan Buddhists, Muktinath-Chumig Gyatsa is a place of [[Dakini]]s, goddesses known as Sky Dancers. It is of great importance for Buddhists that Chumig Gyatsa is one of the 24 [[vajrayana|Tantric]] places.
 
The Tibetan Buddhist tradition states that for this reason Guru Rinpoche, also known as [[Padmasambhava]], the founder of [[Tibetan Buddhism]] meditated at Muktinath on his way to Tibet. It is one of the 51 [[Shakti Peethas|Shakti peetams]].
 
The particular site in the course of the river where the stones become sacred is known as Chakra-Tirtha. The sanctity of this site is said to extend to three yojanas (24 miles) all round.
 
There is a tributary called Chakra-nadi or Jhong Khola that flows from Muktinath and joins the Kali Gandaki at Kagbeni. The entire area (including streams and the mountainside to the north of Muktinath) covers as many as 12 yojanas (96 miles), according to the Puranic account. Among the Saligrama stones, some are from the waters (jalaja) and some are from the mountainside (sthalaja). Puranic texts testify that the sacred stones are what are found in the river and not what are taken out of the rock on its banks.
 
=== Nepali Mandir, Hajipur ===
It is a unique [[Shaivite]] shrine near [[Hajipur]] made in the late medieval period (18th century), by one of the army commanders of Nepal. The temple brings-in a fresh pagoda-style architecture of the Himalayan Kingdom to the plains of the Ganges. This temple is built largely of wood. Another distinctive feature of this temple is its fine wooden carving, which includes, of others, generous erotic scenes.


== Places of archaeological significance ==
== Places of archaeological significance ==
Archaeologically important places around Valmikinagar are [[Lauriya-Nandangarh]] and Someshwar Fort.
[[File:Kali Gandaki River near Marpha, Mustang, Nepal.jpg|thumb|Gandaki River in [[Marpha]], [[Mustang District]], Nepal]]


In Lauria block,<ref name="westchamparan.bih.nic.in">{{cite web |url=http://westchamparan.bih.nic.in/tourist.htm |title=Asking for impossible? |access-date=2 December 2007 |url-status=dead |archive-url=https://archive.today/20110721163350/http://westchamparan.bih.nic.in/tourist.htm |archive-date=21 July 2011 }}</ref> about 1&nbsp;km east of Nandan Garh, a lion pillar of Ashoka, made out of a single block of polished sandstone, measuring {{convert|35|ft|m}} in height with a diameter of 35" at the base and 22" at the top, which is believed to be over 2,300 years old, is in an excellent condition. Its massiveness and exquisite finish furnish striking proof of the skill and resources of the masons of Ashokan age. Two more such pillars with their capitals removed have been discovered in Rampurwa village, close to Gandhi's Bhitiharawa Ashram in Gaunaha block. One of their capitals, the bull is now in the National Museum at New Delhi and the other, the lion, is at Calcutta Museum.
Archaeologically important places around Valmikinagar are [[Lauriya-Nandangarh]] and Someshwar Fort.{{cn|date=October 2024}}
In Lauria block,<ref name="westchamparan.bih.nic.in">{{cite web |url=http://westchamparan.bih.nic.in/tourist.htm |title=Asking for impossible? |access-date=2 December 2007 |url-status=dead |archive-url=https://archive.today/20110721163350/http://westchamparan.bih.nic.in/tourist.htm |archive-date=21 July 2011}}</ref> about 1&nbsp;km east of Nandan Garh, a lion pillar of Ashoka, made out of a single block of polished sandstone, measuring {{convert|35|ft|m}} in height with a diameter of 35" at the base and 22" at the top, which is believed to be over 2,300 years old, is in an excellent condition. Its massiveness and exquisite finish furnish striking proof of the skill and resources of the masons of Ashokan age. Two more such pillars with their capitals removed have been discovered in Rampurwa village, close to Gandhi's Bhitiharawa Ashram in Gaunaha block. One of their capitals, the bull is now in the National Museum at New Delhi and the other, the lion, is at Calcutta Museum.{{cn|date=October 2024}}


At Nandan Garh there are also Baudh ([[Gautama Buddha|Buddha]]) [[stupas]] made out of bricks and about {{convert|80|ft|m}} high which according to the authoritative source are Ashoka Stupas, in which ashes of Lord Buddha's funeral pyre are enshrined.
At Nandan Garh there are also Baudh ([[Gautama Buddha|Buddha]]) [[stupas]] made out of bricks and about {{convert|80|ft|m}} high which according to the authoritative source are Ashoka Stupas, in which ashes of Lord Buddha's funeral pyre are enshrined.{{cn|date=October 2024}}


Someshwar Fort is situated in Narkatiaganj sub-division, near Nepal border, on top of Someshwar Hill at {{convert|2884|ft|m|abbr=on}} altitude. It is in a ruined state but its remains are well defined.
Someshwar Fort is situated in Narkatiaganj sub-division, near Nepal border, on top of Someshwar Hill at {{convert|2884|ft|m|abbr=on}} elevation. It is in a ruined state but its remains are well defined.{{cn|date=October 2024}}


The Bhitiharawa Ashram<ref name="westchamparan.bih.nic.in"/> of [[Mahatma Gandhi]] near Gaunaha in the eastern end of the Valmiki reserve. It is a village in Gaunaha block in Bihar from where Gandhiji started his freedom movement that came to be known as 'Champaran Satyagraha' in India history. The village houses the hut which is called Ashram and has become a place of Gandhian pilgrimage.
The Bhitiharawa Ashram<ref name="westchamparan.bih.nic.in"/> of [[Mahatma Gandhi]] near Gaunaha in the eastern end of the Valmiki reserve. It is a village in Gaunaha block in Bihar from where Gandhiji started his freedom movement that came to be known as 'Champaran Satyagraha' in India history. The village houses the hut which is called Ashram and has become a place of Gandhian pilgrimage.{{cn|date=October 2024}}


=== Mustang Caves ===
=== Mustang Caves ===
{{Main|Mustang Caves}}
{{Main|Mustang Caves}}
[[File:René de Milleville 2.jpg|thumb|300x300px|October 1966- Gandaki Valley, near [[Jomsom|Jomosom]] [[Nepal]], with Tibetan Refugees. Note the head straps for carrying heavy loads. Most Tibetan refugees pass through Nepal to [[India]] where [[14th Dalai Lama|The 14th Dalai Lama]] resides.]]
[[File:René de Milleville 2.jpg|thumb|Gandaki Valley near [[Jomsom]] Nepal in October 1966]]
Mustang caves are a collection of some 10,000 man-made caves dug into the sides of valleys in the [[Mustang District]] of [[Nepal]]. The caves lie on the steep valley walls near the Kali Gandaki River in [[Upper Mustang]]. Several groups of archaeologists and researchers have explored these stacked caves and found partially mummified human bodies and skeletons that are at least 2,000-3,000 years old. Explorations of these caves by conservators and archaeologists have also led to the discovery of valuable religious paintings, sculptures, manuscripts and numerous artifacts belonging to the 12th to 14th century.<ref>{{cite news|url=https://www.theguardian.com/international/story/0,,2072736,00.html |title=Shepherd leads experts to ancient Buddha cave paintings &#124; World news &#124; guardian.co.uk |publisher=Guardian |date= 4 May 2007|access-date=28 November 2009 | location=London | first=Maseeh | last=Rahman}}</ref>
Mustang caves are a collection of some 10,000 human-made caves dug into the sides of valleys in the [[Mustang District]] of [[Nepal]]. The caves lie on the steep valley walls near the Kali Gandaki River in [[Upper Mustang]]. Several groups of archaeologists and researchers have explored these stacked caves and found partially mummified human bodies and skeletons that are at least 2,000-3,000 years old. Explorations of these caves by conservators and archaeologists have also led to the discovery of valuable religious paintings, sculptures, manuscripts and numerous artifacts belonging to the 12th to 14th century.<ref>{{cite news|url=https://www.theguardian.com/international/story/0,,2072736,00.html |title=Shepherd leads experts to ancient Buddha cave paintings &#124; World news &#124; guardian.co.uk |publisher=Guardian |date= 2007|access-date=28 November 2009 |location=London |first=M. | last=Rahman}}</ref>


== Development scenario ==
== Development scenario ==
=== Hydropower development ===
=== Hydropower development ===
==== Nepal ====
==== Nepal ====
In Nepal, Sapta Gandaki alone has a huge hydropower potential of 20,650 MW (economic exploitable potential is 5,270 MW) out of a total estimated potential of 83,290 MW (economically exploitable potential is 42,140 MW). The country has so far been able to generate only around 600 MW of hydropower<ref>{{cite web|url=http://www.nepalnews.com.np/archive/2006/others/feature/sep/news_feature01.php |title=Nepalnews.com Mercantile Connumications Pvt. Ltd |publisher=Nepalnews.com.np |access-date=28 November 2009|archive-url = https://web.archive.org/web/20061007052525/http://www.nepalnews.com.np/archive/2006/others/feature/sep/news_feature01.php |archive-date = 7 October 2006|url-status=dead}}</ref> out of which the Gandak basin projects contribute more than 266 MW, about 44%. The hydropower projects built are the Trisuli at Nuwakot (21 MW), Devighat at Nuwakot (14 MW), Pokhra (1 MW) and Western Gandak HEP, at Nawalparasi (15 MW), Marsyangdi at Tanahu (69 MW), Kali Gandaki at Syanja (144 MW), and Syange (2 MW). Middle Marsyangdi HE Project (70 MW) at Lamjung is under final stage of construction.  Several major projects are on the anvil for implementation in the near future. With Government of Nepal now according priority to private-sector participation in a multi-pronged approach, the pace of hydropower development will get accelerated.{{citation needed|date=June 2019}}
In Nepal, Sapta Gandaki alone has a huge [[hydropower]] potential of 20,650 MW (economic exploitable potential is 5,270 MW) out of a total estimated potential of 83,290 MW (economically exploitable potential is 42,140 MW). The country has so far been able to generate only around 600 MW of hydropower<ref>{{cite web|url=http://www.nepalnews.com.np/archive/2006/others/feature/sep/news_feature01.php |title=Nepalnews.com Mercantile Connumications Pvt. Ltd |publisher=Nepalnews.com.np |access-date=28 November 2009|archive-url = https://web.archive.org/web/20061007052525/http://www.nepalnews.com.np/archive/2006/others/feature/sep/news_feature01.php |archive-date = 7 October 2006|url-status=dead}}</ref> out of which the Gandak basin projects contribute more than 266 MW, about 44%. The hydropower projects built are the Trisuli at Nuwakot (21 MW), Devighat at Nuwakot (14 MW), Pokhra (1 MW) and Western Gandak HEP, at Nawalparasi (15 MW), Marsyangdi at Tanahu (69 MW), Kali Gandaki at Syanja (144 MW), and Syange (2 MW). Middle Marsyangdi HE Project (70 MW) at Lamjung is under final stage of construction.  Several major projects are on the anvil for implementation in the near future. With Government of Nepal now according priority to private-sector participation in a multi-pronged approach, the pace of hydropower development will get accelerated.{{citation needed|date=June 2019}}


A major Indian firm has entered into a share purchase and joint venture agreement with a Nepalese firm to acquire 80 per cent stake of Nepalese Company for development of the Upper Marsyangdi HEP (250MW). Achieving the economically exploitable potential need would no more be a mirage.<ref>{{cite web |url=http://news.webindia123.com/news/Articles/India/20071127/834717.html |title=GMR energy to acquire 80% stake in Nepal's Himtal Power |publisher=News.webindia123.com |date=27 November 2007 |access-date=28 November 2009 |url-status=live |archive-url=https://web.archive.org/web/20120307132138/http://news.webindia123.com/news/Articles/India/20071127/834717.html |archive-date=7 March 2012 }}</ref>
A major Indian firm has entered into a share purchase and joint venture agreement with a Nepalese firm to acquire 80 per cent stake of Nepalese Company for development of the Upper Marsyangdi HEP (250MW). Achieving the economically exploitable potential need would no more be a mirage.<ref>{{cite web |url=http://news.webindia123.com/news/Articles/India/20071127/834717.html |title=GMR energy to acquire 80% stake in Nepal's Himtal Power |publisher=News.webindia123.com |date=27 November 2007 |access-date=28 November 2009 |url-status=live |archive-url=https://web.archive.org/web/20120307132138/http://news.webindia123.com/news/Articles/India/20071127/834717.html |archive-date=7 March 2012 }}</ref>
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== Navigation on the river ==
== Navigation on the river ==
Nepal has carried out studies on the feasibility of having navigational use of the Gandaki river. Studies indicate that (a) it is feasible only in the lower reaches, (b) link it with India's number 1 highway from Allahabad to Haldia, and (c) cognizance has to be taken of the adverse situation which could arise due to increased irrigation use in dry seasons which could restrict the river level for maintaining possible navigation.{{citation needed|date=January 2021}}
Nepal has carried out studies on the feasibility of having navigational use of the Gandaki river. Studies indicate that (a) it is feasible only in the lower reaches, (b) link it with India's number 1 highway from Allahabad to Haldia, and (c) cognizance has to be taken of the adverse situation which could arise due to increased irrigation use in dry seasons which could restrict the river level for maintaining possible navigation.{{citation needed|date=January 2021}}
==In traditional and popular culture==
[[File:Kali River in Ramghat.jpg|thumb|The Gandaki river divides [[Syangja District]] and [[Palpa District]] in Ramghat]]
The Gandaki river is mentioned in the ancient [[Sanskrit]] epic [[Mahabharata]]. Its evolution is described in Shiva Purana, Kumarakhand, in the chapter of the killing of Shankhachuda.{{citation needed|date=June 2022}}
A part of episode 1 of the documentary series "[[The Living Planet]]" was filmed in the [[Kali Gandaki Gorge]].<ref>{{cite AV media |title=The Building of the Earth |people=Kelly, N. (producer) |date=2014 |series=The Living Planet |publisher=BBC Two |url=https://www.bbc.co.uk/programmes/b01qnrbn}}</ref>


==See also==
==See also==
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* [https://web.archive.org/web/20090410061556/http://discoverbihar.bih.nic.in/pages/wildlife.htm WILD LIFE SANCTUARIES AND NATIONAL PARKS]
* [https://web.archive.org/web/20090410061556/http://discoverbihar.bih.nic.in/pages/wildlife.htm WILD LIFE SANCTUARIES AND NATIONAL PARKS]
* [https://web.archive.org/web/20090915182725/http://forest.bih.nic.in/ValmikiSanctuary.htm Valmiki Tiger Reserve]
* [https://web.archive.org/web/20090915182725/http://forest.bih.nic.in/ValmikiSanctuary.htm Valmiki Tiger Reserve]
* [http://news.webindia123.com/news/Articles/India/20071127/834717.html GMR energy to acquire 80% stake in Nepal's Himtal Power]
* [http://news.webindia123.com/news/Articles/India/20071127/834717.html GMR energy to acquire 80% stake in Nepal's Himtal Power] {{Webarchive|url=https://web.archive.org/web/20120307132138/http://news.webindia123.com/news/Articles/India/20071127/834717.html |date=7 March 2012 }}
* [https://web.archive.org/web/20090410061940/http://wrd.bih.nic.in/gandak.html Gandak Barrage]
* [https://web.archive.org/web/20090410061940/http://wrd.bih.nic.in/gandak.html Gandak Barrage]
* [https://web.archive.org/web/20100108190009/http://wrmin.nic.in/index3.asp?subsublinkid=288&langid=1&sslid=369 The India-Nepal Treaty]
* [https://web.archive.org/web/20100108190009/http://wrmin.nic.in/index3.asp?subsublinkid=288&langid=1&sslid=369 The India-Nepal Treaty]

Latest revision as of 15:45, 16 March 2026


Gandaki River
Narayani
From top: Narayani River in Chitwan, Gandak River in Hajipur, Gandak River in Nepal, The Gandak River Barrage in West Champaran Bihar. Anoma River in Buddhist Era
Map showing the Ghaghara and Gandaki tributaries of the Ganges
Location
CountryNepal, India
CitiesLo Manthang, Jomsom, Beni, Baglung, Kusma, Pokhara, Gorkha, Ridi, Devghat, Narayangarh, Valmikinagar, Triveni, Nepal, Hajipur, Sonpur, Muzaffarpur, Bagaha
Physical characteristics
SourceNhubine Himal Glacier
 • locationMustang District, Nepal
 • coordinates29°17′19″N 83°52′39″E / 29.28861°N 83.87750°E / 29.28861; 83.87750
 • elevation6,268 m (20,564 ft)
MouthGanges
 • location
Sonpur, India
 • coordinates
25°39′9″N 85°11′4″E / 25.65250°N 85.18444°E / 25.65250; 85.18444
 • elevation
44 m (144 ft)
Length814 km (506 mi)
Basin size46,300 km2 (17,900 sq mi)
Discharge 
 • average2,025 m3/s (71,500 cu ft/s)
 • minimum500 m3/s (18,000 cu ft/s)
 • maximum30,000 m3/s (1,100,000 cu ft/s)
Basin features
Tributaries 
 • leftTrishuli
 • rightKali Gandaki

The Gandaki River, also known as the Narayani and Gandak, is one of the major rivers in Nepal and a left-bank tributary of the Ganges in India. Its total catchment area is 46,300 km2 (17,900 sq mi), most of it in Nepal. In the Nepal Himalayas, the Gandaki is notable for its deep canyon. The basin also contains three mountains over 8,000 m (26,000 ft), namely Dhaulagiri, Manaslu and Annapurna Massif. Dhaulagiri is the highest point of the Gandaki basin. In its upper reaches, the river is known as Kali Gandaki (or Gandaki) as it flows through the Mustang District and the famous Kali Gandaki Gorge in Nepal. When the river reaches the Terai plains of Nepal, it is referred to as the Narayani River. This name change typically occurs near the confluence with the Trishuli River at Devghat in Chitwan. Upon entering India, the river is known as the Gandak River.

River course[edit | edit source]

Nepal[edit | edit source]

Panorama of the Kali Gandaki gorge in Upper Mustang
River Gandaki in Kagbeni, Nepal

The Kali Gandaki river source is at the border with Tibet at an elevation of 6,268 m (20,564 ft) at the Nhubine Himal Glacier in the Mustang region of Nepal.[1][2]

The headwater stream on some maps is named the Chhuama Khola and then, nearing Lo Manthang, the Nhichung Khola or Choro Khola. The Kali Gandaki then flows southwest (with the name of Mustang Khola on old, outdated maps) through a sheer-sided, deep canyon before widening at the steel footbridge at Chele, where part of its flow funnels through a rock tunnel, and from this point the now wide river is called the Kali Gandaki on all maps. In Kagbeni a major tributary named Johng Khola, Kak Khola or Krishnaa descends from Muktinath.

The river then flows southward through a steep gorge known as the Kali Gandaki Gorge, or Andha Galchi, between the mountains Dhaulagiri, elevation 8,167 m (26,795 ft) to the west and Annapurna, elevation 8,091 m (26,545 ft) to the east. If one measures the depth of a canyon by the difference between the river height and the heights of the highest peaks on either side, this gorge is the world's second deepest after the Yarlung Tsangpo Grand Canyon (ca. 6000 m). The portion of the river directly between Dhaulagiri and Annapurna I, 7 km (4.3 mi) downstream from Tukuche), is at an elevation of 2,520 m (8,270 ft), which is 5,571 m (18,278 ft) lower than Annapurna I. The river is older than the Himalayas. As tectonic activity forces the mountains higher, the river has cut through the uplift. South of the gorge, the river is joined by Rahughat Khola at Galeshwor, Myagdi Khola at Beni, Modi Khola near Kushma and Badigaad at Rudrabeni above Ridi Bazaar. The river then turns east to run along the northern edge of the Mahabharat Range. One of the largest hydroelectricity project in Nepal is located along this stretch of the river. Turning south again and breaking through the Mahabharats, Kali Gandaki is then joined by a major tributary, the Trishuli, at Devghat, which is larger than the Kali Gandaki. Gandaki is then joined by the East Rapti River draining the Inner Terai valley known as Chitwan. The Gandaki then crosses the Sivalik Hills into the Terai plains of Nepal. From Devghat, the river flows southwest of Gaindakot town. The river later curves back towards the southeast as it enters India where it is called the Gandak.

Below Gaindakot the river is known as the Narayani or Sapt Gandaki (Seven Gandakis), for seven tributaries rising in the Himalaya or further north along the main Ganges-Brahmaputra divide. These are the Kali Gandaki, the Trishuli River, and the five main tributaries of the Trishuli known as the Daraudi, Seti, Madi, Marsyandi and Budhi Gandaki.

India[edit | edit source]

The entry point of the river at the Indo–Nepal border is also the confluence called Triveni with the rivers Pachnad and Sonha descending from Nepal. Pandai river flows into Bihar from Nepal in the eastern end of the Valmiki Sanctuary and meets Masan. The Gandak enters India at first in Maharajganj District of Uttar Pradesh for around 25 km (16 mi); it also passes through Kushinagar District before entering Bihar. The Gandak flows southeast 300 km (190 mi) across the Gangetic plain of Bihar state through West Champaran, Gopalganj, East Champaran, Saran, Muzaffarpur and Vaishali districts.[3]

From its exit from the outermost Siwaliks foothills to the Ganga, the Gandak has built an immense megafan comprising Eastern Uttar Pradesh and North Western Bihar in the Middle Gangetic Plains.[4]

Glaciers, glacial lakes and glacial lake outburst floods[edit | edit source]

Glacier lakes, among the most hazardous features of high mountains, are usually formed behind dams of moraine debris left behind by retreating glaciers, a trend that is observed all over the world. Even though glacial lake outburst flood (GLOF) events have been occurring in Nepal for many decades, the Dig Tsho glacier outburst, which took place in 1985, has triggered detailed study of this phenomenon. In 1996, the Water and Energy Commission Secretariat (WECS) of Nepal reported that five lakes were potentially dangerous, namely, Dig Tsho, Imja, Lower Barun, Tsho Rolpa, and Thulagi, all lying above 4,100 m (13,500 ft). A recent study done by ICIMOD and UNEP (UNEP, 2001) reported 27 potentially dangerous lakes in Nepal. In ten of them GLOF events have occurred in the past few years and some have been regenerating after the event.[citation needed]

The Thulagi glacier, located in the Upper Marsyangdi River basin, is one out of the two moraine-dammed lakes that was identified as a potentially dangerous lake as it may outburst.[5]

Important towns[edit | edit source]

Kali Gandaki River near Ghasa, between Annapurna and Dhaulagiri

The important towns in the Indian part of the Gandak river are Valmikinagar (Bhainsalotan) - location of Gandak Barrage, Bagaha, Bettiah (district headquarters & field directorate of Valmiki Tiger Project), Harinagar (Ramnagar), Hajipur (across the Ganges 10  km from Patna) and Sonepur (also Known as Harihar Kshetra), near Patna.[citation needed]

National Parks[edit | edit source]

Chitwan National Park of Nepal and Valmiki National Park of India are adjacent to each other in the vicinity of Valmikinagar around the Gandak Barrage.

Chitwan National Park[edit | edit source]

Chitwan National Park

Chitwan National Park covers an area of 932 square kilometres (360 sq mi). Established in 1973, it is the oldest national park of Nepal. It was granted the status of a World Heritage Site in 1984. It is located in Chitwan, one of the Inner Terai Valleys of Nepal. The park is rich in flora and fauna, including Bengal Tigers and one of the last populations of single-horned Indian rhinoceros (Rhinoceros unicornis). The area used to be known as the Chitwan Valley. It was a place for big game hunting and until 1951 it was a hunting reserve. At the park there is canoeing, elephant rides, and guided jungle walks.

Valmiki National Park[edit | edit source]

Valmiki Sanctuary covers about 800 square kilometres (310 sq mi) of forest and was the 18th tiger reserve established in India.[6] It is ranked fourth in terms density of tiger population. Valmikinagar is located nearly 100 kilometres (62 mi) from Bettiah in the northernmost part of the West Champaran district, Bihar, bordering Nepal. Valmikinagar is a small town with scattered habitation, mostly within the forest area and has a railroad station in the district of West Champaran, close to the railhead of Bagaha. It has diverse landscapes, sheltering rich wildlife habitats and floral and faunal composition with the prime protected carnivores and was included in the National Conservation Programme of the Project Tiger in the year 1994. According to a 1998 report by the Zoological Survey of India, the sanctuary has 53 mammals, 145 birds, 26 reptile and 13 amphibians[7] and a Tiger Reserve.[8]

The notable species of wild fauna include: tiger, leopard, wild dog, wild boar, bison, bear, peacock, partridge, hornbill, hill mynah, woolly-necked stork, python, crocodile, deer, sambar, blue bull, barking deer, hog deer.

As per the Botanical Survey of India report of 1998 there are seven types of vegetation consisting of seven classes of forests; home to 84 species of trees (subtropical trees such as sal, sagwan, bamboo, and cane), 32 shrubs and climbers and 81 herbs and grasses.

Religious significance[edit | edit source]

Muktinath Vaishnava temple idols, Nepal

Between the Dhaulagiri and Annapurna mountain ranges, the Gandaki River flows through the village of Muktinath and by the Ashram of Pulaha. In ancient times, the mountain range surrounding Pulaha was called Salagiris due to the vast forests of sal trees. The stones found in this region are therefore called Saligrama – Silas. It has great significance to Hindus, particularly to Brahmins. Smarthas uses this as the replica of lord Narayana. Srivaisnavas, and Madhvacharya sects who consider the place where one can find saligrama silas in the river bed of the Gandaki River, and the Mukthinath temple as one of the 108 Divyakshetrams.[9]

Places of archaeological significance[edit | edit source]

Gandaki River in Marpha, Mustang District, Nepal

Archaeologically important places around Valmikinagar are Lauriya-Nandangarh and Someshwar Fort.[citation needed] In Lauria block,[10] about 1 km east of Nandan Garh, a lion pillar of Ashoka, made out of a single block of polished sandstone, measuring 35 feet (11 m) in height with a diameter of 35" at the base and 22" at the top, which is believed to be over 2,300 years old, is in an excellent condition. Its massiveness and exquisite finish furnish striking proof of the skill and resources of the masons of Ashokan age. Two more such pillars with their capitals removed have been discovered in Rampurwa village, close to Gandhi's Bhitiharawa Ashram in Gaunaha block. One of their capitals, the bull is now in the National Museum at New Delhi and the other, the lion, is at Calcutta Museum.[citation needed]

At Nandan Garh there are also Baudh (Buddha) stupas made out of bricks and about 80 feet (24 m) high which according to the authoritative source are Ashoka Stupas, in which ashes of Lord Buddha's funeral pyre are enshrined.[citation needed]

Someshwar Fort is situated in Narkatiaganj sub-division, near Nepal border, on top of Someshwar Hill at 2,884 ft (879 m) elevation. It is in a ruined state but its remains are well defined.[citation needed]

The Bhitiharawa Ashram[10] of Mahatma Gandhi near Gaunaha in the eastern end of the Valmiki reserve. It is a village in Gaunaha block in Bihar from where Gandhiji started his freedom movement that came to be known as 'Champaran Satyagraha' in India history. The village houses the hut which is called Ashram and has become a place of Gandhian pilgrimage.[citation needed]

Mustang Caves[edit | edit source]

Gandaki Valley near Jomsom Nepal in October 1966

Mustang caves are a collection of some 10,000 human-made caves dug into the sides of valleys in the Mustang District of Nepal. The caves lie on the steep valley walls near the Kali Gandaki River in Upper Mustang. Several groups of archaeologists and researchers have explored these stacked caves and found partially mummified human bodies and skeletons that are at least 2,000-3,000 years old. Explorations of these caves by conservators and archaeologists have also led to the discovery of valuable religious paintings, sculptures, manuscripts and numerous artifacts belonging to the 12th to 14th century.[11]

Development scenario[edit | edit source]

Hydropower development[edit | edit source]

Nepal[edit | edit source]

In Nepal, Sapta Gandaki alone has a huge hydropower potential of 20,650 MW (economic exploitable potential is 5,270 MW) out of a total estimated potential of 83,290 MW (economically exploitable potential is 42,140 MW). The country has so far been able to generate only around 600 MW of hydropower[12] out of which the Gandak basin projects contribute more than 266 MW, about 44%. The hydropower projects built are the Trisuli at Nuwakot (21 MW), Devighat at Nuwakot (14 MW), Pokhra (1 MW) and Western Gandak HEP, at Nawalparasi (15 MW), Marsyangdi at Tanahu (69 MW), Kali Gandaki at Syanja (144 MW), and Syange (2 MW). Middle Marsyangdi HE Project (70 MW) at Lamjung is under final stage of construction. Several major projects are on the anvil for implementation in the near future. With Government of Nepal now according priority to private-sector participation in a multi-pronged approach, the pace of hydropower development will get accelerated.[citation needed]

A major Indian firm has entered into a share purchase and joint venture agreement with a Nepalese firm to acquire 80 per cent stake of Nepalese Company for development of the Upper Marsyangdi HEP (250MW). Achieving the economically exploitable potential need would no more be a mirage.[13]

Reportedly there are several other major projects being pursued by the Government of Nepal for private sector participation on IPP basis.[citation needed]

Irrigation[edit | edit source]

The Gandak Project at Valmikinagar (Bhainsaloton) intercepts water of a catchment area of 37,410 km (23,250 mi), which is mostly in Nepal and partly in India. An agreement was signed on 4 December 1959 between the governments of Nepal and of India on the Gandak Irrigation and Power Project. It encompassed the construction of a barrage, canal head regulators and other appurtenant works about 33 m (108 ft) below the existing Triveni Canal Head Regulator.[14] The agreement was modified in 1964 for the protection of Nepal's riparian rights. Basically there is an agreed share of water for ‘western canal system including a power station in Nepal and eastern canal system. As a part of this bilateral agreement, the Gandak Barrage, a part of Gandak Project, was built in 1968–69 over the Gandak river for providing irrigation to Nepal, Uttar Pradesh and Bihar.[15] The irrigation potential of this project is 11,510 km2 (4,440 sq mi), spread in the district of West Champaran, East Champaran, Muzaffarpur, Samastipur, Saran, Siwan and Gopalganj. The Eastern Gandak Canal Project was taken up in 1960 and Main Canal system was completed in 1975 for flow irrigation in Nepal for the gross commanded area estimated to be 103,500 acres (419 km2).[16]

A Gandak Hydropower Station with an installed capacity of 15 MW has also been constructed and commissioned on the bypass to Eastern Gandak Canal.[17]

Flood management[edit | edit source]

Flood management does not aim at total elimination or control of floods or providing total immunity from the effects of all magnitudes of floods, which is neither practicable from economic considerations nor even necessary, keeping in view other realities that are faced in the Indian context. Thus, a multi-pronged strategy ranging from modifying the floods by means of structural measures to learning to live with the floods by means of other non-structural measures is the goal of flood management. Measures for protection against extreme floods of low frequency are seldom economically feasible. The term "flood management" refers to the provision of a reasonable degree of protection against floods by measures to mitigate the recurring havoc caused by floods. This is what is being done in flood plains of Gandak River in Bihar and Uttar Pradesh which are affected by floods.[18]

Navigation on the river[edit | edit source]

Nepal has carried out studies on the feasibility of having navigational use of the Gandaki river. Studies indicate that (a) it is feasible only in the lower reaches, (b) link it with India's number 1 highway from Allahabad to Haldia, and (c) cognizance has to be taken of the adverse situation which could arise due to increased irrigation use in dry seasons which could restrict the river level for maintaining possible navigation.[citation needed]

In traditional and popular culture[edit | edit source]

The Gandaki river divides Syangja District and Palpa District in Ramghat

The Gandaki river is mentioned in the ancient Sanskrit epic Mahabharata. Its evolution is described in Shiva Purana, Kumarakhand, in the chapter of the killing of Shankhachuda.[citation needed] A part of episode 1 of the documentary series "The Living Planet" was filmed in the Kali Gandaki Gorge.[19]

See also[edit | edit source]

References[edit | edit source]

  1. Upper& Lower Mustang (Map). 1:70000. Kathmandu: Nepal Map Publisher Pvt., Ltd.
  2. Garzione, C. N.; Quade, J.; DeCelles, P.G. & English, N.B. (2000). "Predicting paleoelevation of Tibet and the Himalaya from δ18O vs. altitude gradients in meteoric water across the Nepal Himalaya". Earth and Planetary Science Letters. 183 (1–2): 215–229. Bibcode:2000E&PSL.183..215G. doi:10.1016/S0012-821X(00)00252-1.
  3. "River Basin". Flood Management Improvement Support Centre, Water Resources Department of Government of Bihar. Retrieved 7 March 2024.
  4. "hydro-india-other". Industcards.com. Retrieved 28 November 2009.{{cite web}}: CS1 maint: deprecated archival service (link)
  5. "BGR/NLfB/GGA: Gletschersee Thulagi". Bgr.de. Archived from the original on 18 July 2011. Retrieved 28 November 2009.
  6. "Valmiki National Park". The Hindu. 7 May 2007. Archived from the original on 12 January 2016. Retrieved 25 October 2014.
  7. "Wildlife Sanctuaries". Archived from the original on 10 April 2009. Retrieved 3 December 2007.
  8. "Valmiki Sanctuary". Forest.bih.nic.in. Archived from the original on 15 September 2009. Retrieved 28 November 2009.
  9. "108divyakshetrams". Archived from the original on 24 December 2007. Retrieved 30 November 2007.
  10. 10.0 10.1 "Asking for impossible?". Retrieved 2 December 2007.{{cite web}}: CS1 maint: deprecated archival service (link)
  11. Rahman, M. (2007). "Shepherd leads experts to ancient Buddha cave paintings | World news | guardian.co.uk". London: Guardian. Retrieved 28 November 2009.
  12. "Nepalnews.com Mercantile Connumications Pvt. Ltd". Nepalnews.com.np. Archived from the original on 7 October 2006. Retrieved 28 November 2009.
  13. "GMR energy to acquire 80% stake in Nepal's Himtal Power". News.webindia123.com. 27 November 2007. Archived from the original on 7 March 2012. Retrieved 28 November 2009.
  14. "Ministry of Water Resources". Wrmin.nic.in. Archived from the original on 8 January 2010. Retrieved 28 November 2009.
  15. "Commissioned Projects of BHPC". Bshpcltd.com. Archived from the original on 30 April 2009. Retrieved 28 November 2009.
  16. "Gandak barrage". Archived from the original on 10 April 2009. Retrieved 10 April 2009.
  17. Agreement Between His Majesty's Government of Nepal and the Government of India on the Gandak Irrigation and Power Project. Archived 7 August 2008 at the Wayback Machine
  18. "Working Group report on Water Resources" (PDF). Archived from the original (PDF) on 20 February 2009. Retrieved 28 November 2009.
  19. Kelly, N. (producer) (2014). The Building of the Earth. The Living Planet. BBC Two.
  • India's Water Wealth (1975, Dr. K.L.Rao, Orient Longman Ltd, Hyderabad, New Delhi
  • "Waters of Hope" (1993), B.G.Vargehese, New Delhi
  • A Framework for Sustainable Development of the Ganges- Brahmaputra- Meghna (GBM Region), Proceedings of Conference held in Dhaka, 4–5 December 1999–Nepal Water Vision in the GBM Regional Framework, Institute for Integrated Studies, Kathmandu).

External links[edit | edit source]

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