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The Shashe River (or Shashi River) is a major left-bank tributary of the Limpopo River in Zimbabwe. It rises northwest of Francistown, Botswana and flows into the Limpopo River where Botswana, Zimbabwe and South Africa meet.[2] The confluence is at the site of the Greater Mapungubwe Transfrontier Conservation Area.

Shashe River
Shashe River at Shashi Irrigation Scheme, Zimbabwe
Location
CountryBotswana, Zimbabwe
Physical characteristics
Source 
  locationnorthwest of Francistown, Botswana
Mouth 
  location
Limpopo River
Discharge 
  average462 million cubic metres per year (14.6 m3/s; 517 cu ft/s)[1]
Basin features
Tributaries 
  leftTati River, Ramokgwebana River, Thuli
Location of the mouth of the Shashe River on the Limpopo River 22.187961°S 29.354769°E / -22.187961; 29.354769

Hydrology


The Shashe River is a highly ephemeral river, with flow generally restricted to a few days of the year. The river contributes 12.2% of the mean annual runoff of the Limpopo Basin.[3]

Major tributaries of the Shashe River include the Simukwe, Shashani, Thuli, Tati and Ramokgwebana rivers. The lower Shashe is a sand filled channel, with extensive alluvial aquifers in the river channel and below the alluvial plains. These supply water for a number of irrigation schemes including Sibasa and Shashi.

More than two million years ago, the Upper Zambezi River used to flow south through what is now the Makgadikgadi Pan (presently a vast seasonal wetland) to the Shashe River and thence the Limpopo River.


Settlements


There is a road bridge and a rail bridge south of Francistown. The lower Shashe River forms the border between Botswana and Zimbabwe and is unbridged. However, at Tuli, both sides of the river are in Zimbabwe and there are two legal crossing points. The Shashi runs through the Shashi Irrigation Scheme and the Tuli Block.[citation needed]


Dams


The Shashe River at the confluence with the Limpopo Rivers in Botswana
The Shashe River at the confluence with the Limpopo Rivers in Botswana

The Shashe River is dammed near Francistown at Shashe Dam. The original purpose was to supply water to the industrial city of Selebi-Phikwe.[4] In 1982 it was found that groundwater from the local wells in Francistown had high levels of nitrate, and was also inadequate to meet public demand, so the public water supply for that city was changed over to using water from the Shashe Dam.[5] The dam also supplies water to surrounding villages, Phoenix Mine (Tati Nickel Mining Company/Norilsk Nickel) and Mupane Gold Mine (IAMGOLD).[citation needed]

Further downstream, the Dikgatlhong Dam impounds the Shashe near the village of Robelela, completed in December 2011.[6] When full it will hold 400,000,000 cubic metres (1.4×1010 cu ft). The next largest dam in Botswana, the Gaborone Dam, has capacity of 141,000,000 cubic metres (5.0×109 cu ft).[7] A pipeline from the Dikgatlhong Dam will connect to the North-South Carrier (NSC) pipeline at the BPT1 break pressure tank at Moralane. The NSC will take the water south to Gaborone.[8]


See also



References


Citations

  1. A.H.M. Görgens and R.A. Boroto. 1997
  2. Shashe Sub-basin Archived 2012-10-31 at the Wayback Machine
  3. Görgens & Boroto 1997.
  4. Knight 1990, p. 402.
  5. Schmoll 2006, p. 284.
  6. Modikwa 2011.
  7. Dikgatlhong dam - Jeffares & Green.
  8. Paya, Matsiara, Bettesworth, et al. 2012, p. 3.

Sources


На других языках


[de] Shashe

Der Shashe ist ein Grenzfluss zwischen Botswana und Simbabwe.
- [en] Shashe River

[ru] Шаше

Шаше[1][2] (тсвана Noka ya Shashe, англ. Shashe River) — река на востоке Ботсваны и юго-западе Зимбабве. Крупный левый приток реки Лимпопо. Берёт начало вблизи города Франсистаун и течёт в юго-восточном направлении вплоть до своего устья близ границы с ЮАР[3]. На большей части своего течения формирует границу между Ботсваной и Зимбабве. Близ деревни Тули река на коротком участке полностью выходит на территорию Зимбабве, однако вскоре вновь возвращается на границу. Шаше является временной рекой и полностью пересыхает на протяжении большей части года. Шаше составляет 12,2 % от всего поверхностного стока в бассейн Лимпопо[4].



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