Leimatak River

Coordinates: 24°49′20″N 93°30′22″E / 24.8223°N 93.5062°E / 24.8223; 93.5062
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Leimatak
Leimata
Leimatak River is located in Manipur
Leimatak River
Leimatak River is located in India
Leimatak River
Location
CountryIndia
StateManipur
Physical characteristics
SourceMamun Lhang peak
 • locationChurachandpur district
 • coordinates24°23′06″N 93°32′46″E / 24.385°N 93.546°E / 24.385; 93.546 (Mamun Lhang)
 • elevation1,699 metres (5,574 ft)
2nd sourceNungsai hills
 • locationChurachandpur district
 • coordinates24°33′29″N 93°32′06″E / 24.558°N 93.535°E / 24.558; 93.535 (Nungsai)
 • elevation1,692 metres (5,551 ft)
MouthIrang
 • location
near Tamlok, Tamenglong district
 • coordinates
24°49′20″N 93°30′22″E / 24.8223°N 93.5062°E / 24.8223; 93.5062
 • elevation
250 metres (820 ft)
Length74.6 km (46.4 mi)
Basin size627 km2 (242 sq mi)
Basin features
ProgressionIrang, Barak
River systemBrahmaputra
Tributaries 
 • leftThingbong
 • rightTalai, Iring

The Leimatak River (or Leimata River)[1] is an upstream tributary of the Barak River in Manipur, India. It originates in the Churachandpur district near the Mamun Lhang peak (or Khaorang peak), and flows north for 34 km (21 mi) before entering the Noney district. After flowing an equal amount of distance in the Noney district, it enters the Tamenglong district, where it drains into the Irang River, a major tributary of the Barak River.[2]

Course[edit]

The Mamun Lhang peak (1,699 m) is on a mountain range to the west of the Thangjing Hills range, running roughly parallel to it. The main head stream of Leimatak River, called Tuibin river, comes down from the peak on its west, flowing north. A second head stream, called Thingbong, flows south fom the hills around the Nungsai peak (1,692 m). The two streams meet near the Thangsi village and form the Leimatak River, flowing due northeast.

A tributary called Talai flows parallel to Tuibin/Leimatak, east of the Mamun Lhang range and west of the Thangjing Hills range collecting drainage from both.

The combined river flows northeast till the base of the Thangjing Hills range, and turns northwest, near the village of L. Phaikholum. The Leimatak Power Station is located here. Also called the "Loktak Power Station", it is powered by water from the eastern slopes of the Thangjing Hills range, via a pipeline that is tunnelled through the hills. These waters would have flowed into the Loktak Lake, but now they are released into the Leimatak River after their usage for power generation.[3][4]

Near the Pinjang village in the Noney district, the Cachar–Bishnupur Road (or "Old Cachar Road") crosses the Leimatak River. The bridge is known as the Leimatak Bridge, and the locality itself is called "Leimatak" in historical documents.

Near Awangkhal, a tributary called Iring joins the Leimatak River, which flows down from Noney in the northeast. The combined river flows west in the channel of Iring to join the Irang River near Tamlok. The Cachar-Imphal Road (or "New Cachar Road", part of National Highway 37) runs in the valley of Iring, crossing the Irang River close to the confluence with Leimatak.

The overall length of the river is 74.6 km (46.4 mi) and the basin area is 627 km2 (242 sq mi).[5]

History[edit]

The Old Cachar Road was the primary travel route between Manipur and the Indian plains. It was traversed often by traders, travellers, troops, as well as the rulers when they fled Burmese occupation. In one of the first such events, the ruler Ching-Thang Khomba (also called Bhagyachandra or Jai Singh, r. 1759–1798) fled Manipur during a Burmese occupation and used Cachar as his base. He is said to have made four attempts to oust the Burmese between 1775 and 1782, but beaten back each time. After 1782, the Burmese withdrew and left the kingdom to the ruler.[6]

Even 1786, the Ching-Thang Khomba mobilised his forces to attack the Kuki tribes to the west of the Leimatak River valley, based at a village called "Khongchai" in the Tuipui River valley.[a] The forces travelled up the Leimatak River valley up to a location called the Kuchu valley in the Tuibin headstream (at coordinates 24°26′57″N 93°32′36″E / 24.44917°N 93.54333°E / 24.44917; 93.54333 (Kuchu valley) estimated by the Kuki Research Forum scholars), where they made their base. They also constructed a temporary royal residence there. From this base, they attacked the Khongjai villages (Kuki villages) in the Tuipui river valley across the hill range to the west.[1][7] The name "Kuchu" was apparently reused to name the king's court in the Kangla Complex, probably in remembrance of the victory over the Khongjais.[8]

After Manipur became a British protectorate, c. 1830, a frontier military post of Manipur was located at "Leimatak", possibly at the crossing of the Old Cachar Road. Other posts in the west were at the Khoupum valley and "Moirung Hills" (Thangjing Hills).[9]

Notes[edit]

  1. ^ Tuipui river is another tributary of the Irang River that flows north, parallel to the Leimatak River.

References[edit]

  1. ^ a b Kuki Research Forum on objective historical position of the Kukis in Manipur, Ukhrul Times, 25 May 2022.
  2. ^ Churachandpur District Census Handbook (2011), p. 25.
  3. ^ LOKTAK power station - India, globecountries.com, retrieved 10 March 2024.
  4. ^ Ghosh Roy, M.; Virmani, R. G., "Monitoring long term movement of hillslope and stability measures adopted in penstock area of Loktak power station", Journal of Engineering Geology, 1 (1): 255–271
  5. ^ Girija Devi, E.; Debojit Singh, Ch.; Kushwaha, R.A.S. (1997), "Geomorphic Sub-Division of Leimatak Basin, Manipur", The North Eastern Geographer, Volume 28, North East India Geographical Society, p. 26
  6. ^ Harvey, History of Burma (1925), pp. 261–262.
  7. ^ Parratt, The Court Chronicle, Vol. 2 (2009), pp. 25–26.
  8. ^ Parratt, The Court Chronicle, Vol. 2 (2009), p. 134.
  9. ^ Pau, Pum Khan (2019), Indo-Burma Frontier and the Making of the Chin Hills: Empire and Resistance, Taylor & Francis, p. 67, Table 3.1, ISBN 9781000507454

Bibliography[edit]

External links[edit]