Chindwin River

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Chindwin River
  • Burmese: ချင်းတွင်းမြစ်
  • Meitei: ꯅꯤꯡꯊꯤ ꯇꯨꯔꯦꯜ
Homalin aerial.jpg
The Chindwin at Homalin. The smaller, meandering Uyu River can be seen joining the Chindwin.
Irrawaddyrivermap.jpg
Location
Country Myanmar
Physical characteristics
Source 
  location Hukawng Valley, Kachin State
  coordinates 27°3′26.7048″N97°1′33.618″E / 27.057418000°N 97.02600500°E / 27.057418000; 97.02600500
  elevation1,134 m (3,720 ft)
Mouth  
  location
Irrawaddy River
  coordinates
21°28′26″N95°16′53″E / 21.47389°N 95.28139°E / 21.47389; 95.28139
  elevation
55 m (180 ft)
Length1,207 km (750 mi)
Basin size114,684.9 km2 (44,280.1 sq mi) [1]
Discharge 
  locationNear mouth
  average(Period: 1967– 2009)149.7 km3/a (4,740 m3/s) [2]
Discharge 
  location Monywa (74 km upstream of mouth; Basin size: 110,350 km2 (42,610 sq mi)
  average(Period: 1966–2009)4,637 m3/s (163,800 cu ft/s) [2]
  minimum(Period: 1966–2009)649 m3/s (22,900 cu ft/s) [2]
  maximum(Period: 1966–2009)19,935 m3/s (704,000 cu ft/s) [2]
Discharge 
  location Hkamti (Basin size: 27,420 km2 (10,590 sq mi)
  average(Period: 1972–2009)2,290 m3/s (81,000 cu ft/s) [2]
  minimum(Period: 1972–2009)109 m3/s (3,800 cu ft/s) [2]
  maximum(Period: 1972–2009)14,150 m3/s (500,000 cu ft/s) [2]
Basin features
Tributaries 
  left Uyu
  right Myittha

The Chindwin River (Burmese pronunciation: [t͡ɕɪ́ɰ̃dwɪ́ɰ̃mjɪʔ] ), also known as the Ningthi River [3] [4] [5] [6] (Meitei: [niŋtʰituɾel] ), is a river in Myanmar and the largest tributary of the Irrawaddy River, which itself is the principal river of Myanmar. [7]

Contents

Sources

The Chindwin originates in the broad Hukawng Valley of Kachin State of Burma, roughly 26°26′18″N96°33′32″E / 26.43833°N 96.55889°E / 26.43833; 96.55889 , where the Tanai, the Tabye, the Tawan, and the Taron (also known as Turong or Towang) rivers meet.

The headwaters of the Tanai are at 25°30′N97°0′E / 25.500°N 97.000°E / 25.500; 97.000 on the Shwedaunggyi peak of the Kumon range, 12 miles (19 km) north of Mogaung. It flows due north until it reaches the Hukawng Valley. In 2004, the government established the world's largest tiger preserve in the Hukawng Valley, the Hukaung Valley Wildlife Sanctuary, with an area of approximately 6,500 km2 (2,500 sq mi); later, the Sanctuary was extended to 21,800 square kilometres (8,400 sq mi), making it the largest protected area in mainland Southeast Asia. The river then turns to the west and flows through the middle of the plain, [7] joined by the Tabye, the Tawan, and the Taron rivers from the right bank. These rivers drain the mountain ranges to the north and northeast of the Hukawng valley.

Course

The Tanai exits the Hukawng valley through the Taron or Turong valley and through a sharp defile in the river. It then takes on the name of Chindwin, and maintains a general southerly course. [7] It passes the town of Singkaling Hkamti on the left bank, then the town of Homalin, also on the left bank.

The river's course is generally southwesterly until the town of Mingin. It then takes a more southeasterly course entering the broad central plain, passing the city of Monywa on the left bank. Its course at this point forms the boundary between the Sagaing District of Sagaing Region and the Pakokku District of Magway Region.

It enters the Ayeyarwady River (Irrawaddy) at about 21°30′N95°15′E / 21.500°N 95.250°E / 21.500; 95.250 . The extreme outlets into the Ayeyarwady are about 22 miles (35 km) apart, the interval forming a succession of long, low, partially populated islands. The lowest mouth of the Chindwin is, according to tradition, an artificial channel, cut by one of the kings of Bagan (Pagan). It was choked up for centuries until 1824 when it was opened out by an exceptional flood. [8] Satellite pictures show this lowest channel to be the widest one today. [9]

Discharge

Average, minimum and maximum discharge of the Chindwin River at Monywa. Period from 1966/01/01 to 2023/12/31: [2] [10] [11]

YearDischarge (m3/s)YearDischarge (m3/s)
MinMeanMax MinMeanMax
19666105,61124,55019956844,97720,680
19677754,81217,74019966163,98916,080
19687575,13725,45019974324,43420,400
19695824,00620,13019987365,11319,600
19705484,77519,79019994805,18821,530
19715095,79219,45020006325,51418,740
19727573,25716,49020015124,27814,040
19735305,10321,70020026724,59524,300
19749215,56625,00020037445,13418,460
19757094,49317,84020046085,86219,770
19768926,92826,65020055523,48616,200
19777984,39823,80020062423,77116,520
19786723,95616,54020073185,35519,740
19795304,06318,92020082884,50023,270
19808065,07520,30020092573,23216,160
19817903,83316,01020101213,89813,787
19826504,38523,16020111323,77119,673
19836534,24718,84020123434,81716,600
19846005,09122,71020132014,23616,560
19856135,30519,45020142973,16918,081
19865913,98115,42020154,58525,510
19876595,33920,01020168025,16019,067
19886105,09725,45020176,77621,831
19897834,79622,49020185,61819,019
19909075,67020,58020194774,29012,963
19918526,48825,60020206,11417,800
19921,0394,10214,47020212764,77616,610
19939814,82621,14020229724,60311,805
19946443,43913,41020231564,20414,527


Tributaries

  1. Uyu River is the largest tributary joining the Chindwin river just below Homalin on the left. The famous jade mines at Hpakant lie in the headwaters of the Uyu. [12] [13]
  2. Myittha River drains the Kale valley and joins on the right further downstream. The town of Kalewa is on the left bank of their confluence.
  3. Tizu River originates from central Nagaland in northeast India. It flows through Zünheboto and Phek districts and finally joins the Chindwin river.[ citation needed ]

Towns

River Chindwin at Monywa R Chindwin.JPG
River Chindwin at Monywa
1980: River Chindwin 30 km NE of Monywa with Lower Chindwin crater lake Aerial view of lower Chindwin River and Twin Taung (1980).JPG
1980: River Chindwin 30 km NE of Monywa with Lower Chindwin crater lake
  1. Hkamti
  2. Htamanthi
  3. Homalin
  4. Mawlaik
  5. Kalewa
  6. Kalaymyo
  7. Mingin
  8. Monywa [14]

Environment

Much of Chindwin's course lies within mountain ranges and forests. Due to the difficulty of access, much of it remains unspoilt. The government of Burma recently created a very large (2,500 square mile) sanctuary for the endangered tiger within the Hukawng Valley. [15]

History

The mountain ranges to the west of the Chindwin are formidable, yet not totally impregnable to armies. The Kabaw valley saw many an invasion by the kingdom of Manipur to the west, most notably during the reign of King Garibaniwaj (1709–1748) when his army crossed over the Chindwin and the Mu, took Myedu, and reached as far as Sagaing opposite the capital Ava. The tables were turned in 1758 after King Alaungpaya ascended the Burmese throne. [16] The Burmese army invaded and occupied Manipur and Assam marching across the western mountain ranges, and even encroached upon British India.

During World War II, when the Japanese had cut off sea access, the British army and other Allied forces under General Joseph Stilwell retreated on foot to India across the same mountains, with disastrous results, mainly due to disease and hunger. The Ledo Road was built across the Hukawng valley to supply China. [17] The Chindwin was a major barrier both for the Japanese trying to invade India and for the Allied forces attempting to reoccupy Burma. [18]

Ethnography and culture

The chindwin river has a great impact on the culture of western Burma. [19] Central Sino-Tibetan languages originated from valley areas of this river.

Economics

The Chindwin is served by regular river-going vessels up to the town of Homalin. Teak forests within its drainage area have been a valuable resource since ancient times. The Hukawng Valley is known for its abundance of Burmese amber. Along the river, there are deposits of jade, but Hpakant in the headwaters of the Uyu river is the only place in the world where the finest jade - known as jadeite or imperial jade - is found, along with an abundance of fish. [12] [13]

Notes

    References

    1. "Chindwin".
    2. 1 2 3 4 5 6 7 8 Chikamori, Hidetaka; Liu, Heng; Daniell, Trevor. Myanmar 1. Chindwin River (PDF).
    3. Pemberton, R. B. (1835). Report On The Eastern Frontier Of British India. Baptist Mission Press, Kolkata. pp. 19–20.
    4. McCulloch, W.M. (1859). Account of the Valley of Munnipore and of the Hill Tribes; with a Comparative Vocabulary of the Munnipore and other Languages. Calcutta: Bengal Printing Company Limited. pp. 8–40.
    5. Siṃha, K. M. (1989). Hijam Irabot Singh and Political Movements in Manipur. B.R. Publishing Corporation. ISBN   978-81-7018-578-9.
    6. "GENERAL / LATEST NEWS: ENVIS Centre, Ministry of Environment, Forest & Climate Change, Govt. of India". manenvis.nic.in. Ministry of Environment, Forest and Climate Change, Government of India. National Informatics Centre . Retrieved 2023-03-25.{{cite web}}: CS1 maint: others (link)
    7. 1 2 3 Chisholm, Hugh, ed. (1911). "Chindwin"  . Encyclopædia Britannica . Vol. 6 (11th ed.). Cambridge University Press. p. 232.
    8. "Chindwin River". Encyclopædia Britannica online. Retrieved 2008-10-07.
    9. "Earth from Space". NASA, November 1998. Archived from the original on 2007-08-02. Retrieved 2008-10-07.
    10. "River Discharge and Reservoir Storage Changes Using Satellite Microwave Radiometry".
    11. "The Flood Observatory".
    12. 1 2 "Hpakan Other Rock Mine(Myanmar)". aditnow.co.uk. Archived from the original on 2011-07-19. Retrieved 2008-12-27.
    13. 1 2 Richard W. Hughes; Fred Ward. "Heaven and Hell: The Quest for Jade in Upper Burma". Ruby-Sapphire.com. Archived from the original on 2009-02-05. Retrieved 2008-12-27.
    14. "Map of Sagaing Division". Asterism. Retrieved 2008-10-07.
    15. "Rationale for a National Tiger Action Plan for Myanmar" (PDF). Wildlife Conservation Society (WCS). Archived from the original (PDF) on 2009-02-26. Retrieved 2008-12-27.
    16. Phanjoubam Tarapot (2003). Bleeding Manipur. Har-Anand Publications. pp. 112–3. ISBN   978-81-241-0902-1 . Retrieved 2008-11-19.
    17. Baruah, Sri Surendra. "The Stillwell Road A Historical Review". Tinsukia. Archived from the original on 2008-10-13. Retrieved 2008-11-19.
    18. "Chindwin River". The Pacific War Online Encyclopaedia. Retrieved 2008-10-07.
    19. Andrew Hsiu which taken from a journal titled "Morphological Evidence for a Central Branch of Trans-Himalayan (Sino-Tibetan)." by Scott DeLancey which was published on 2015

    Bibliography