Shashe River

Shashe River
Physical characteristics
Mouth	Limpopo River

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Location of the mouth of the Shashe River on the Limpopo River 22.187961°S 29.354769°E / -22.187961; 29.354769

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. The confluence is at the site of the Greater Mapungubwe Transfrontier Conservation Area.

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.

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.

Dams

The Shashe River is dammed near Francistown at Shashe Dam. The original purpose was to supply water to the industrial city of Selebi-Phikwe. 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. The dam also supplies water to surrounding villages, Phoenix Mine (Tati Nickel Mining Company/Norilsk Nickel) and Mupane Gold Mine (IAMGOLD).

Further downstream, the Dikgatlhong Dam impounds the Shashe near the village of Robelela, completed in December 2011. 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). 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.

See also

• Geological changes to the course of the Zambezi River
• Thuli River
• Mchabezi River

References

Citations

Sources

• "Dikgatlhong dam". Jeffares & Green. Retrieved 2012-09-21.
• Knight, D.J. (1990-06-01). "The proven usefulness of instrumentation systems on varied dam projects". Geotechnical Instrumentation in Practice: Purpose, Performance and Interpretation : Proceedings of the Conference Geotechnical Instrumentation in Civil Engineering Projects. Thomas Telford. ISBN 978-0-7277-1515-9. Retrieved 2012-09-18. {{cite book}}: Invalid |ref=harv (help)
• Modikwa, Onalenna (13 December 2011). "Dikgatlhong dam complete ahead of schedule". Mmegi. Retrieved 2012-09-21. {{cite web}}: Invalid |ref=harv (help)
• B. Paya, G.T. Matsiara, I.J. Bettesworth, M. van der Walt, P. du Plessis, B. Bosman, D. Stephenson, N. Mbayi, A. Keabetswe (2012). "BOTSWANA'S NORTH SOUTH CARRIER 2 WATER TRANSFER SCHEME" (PDF). WISA 2012 conference. Retrieved 2012-09-22.{{cite web}}: CS1 maint: multiple names: authors list (link)
• Schmoll, Oliver (2006). Protecting Groundwater for Health: Managing the Quality of Drinking-Water Sources. World Health Organization. p. 284. ISBN 978-92-4-154668-3. Retrieved 2012-09-18. {{cite book}}: Invalid |ref=harv (help)
• Görgens, A.H.M.; Boroto, R.A. (1997). "River: flow balance anomalies, surprises and implications for integrated water resources management". Proceedings of the 8th South African National Hydrology Symposium, Pretoria, South Africa.