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Int J Earth Sci 100:323–354, Frimmel HE et al (2013) A new lithostratigraphic subdivision and geodynamic model for the Pan-African western Saldania Belt, South Africa. Trans Geol Soc S Afr 18(1915):72–101, Rooney AD et al (2015) A Cryogenian chronology: two long-lasting synchronous Neoproterozoic glaciations. The host carbonate succession (Otavi Group) forms part of an extensive platform on the northern margin of the Khomas Trough, which is believed to be an equivalent to the Gariep Basin in the Damara Belt. Study Guide for Pretoria University. These units grade into a second, regionally extensive sheet of glaciogenic diamictite with minor intercalated banded iron formation. Many of the modern surnames in the dictionary can be traced back to Britain and Ireland. The river was named the Orange River by Colonel Robert Gordon, commander of the United East India Company (VOC) garrison at Cape Town, on a trip to the interior in 1779. Major Hydropower Installations in the Basin • Gariep Dam: –Full capacity: 360 MW • Vanderkloof Dam –Full capacity: 240 MW • ‘Muela Hydroelectric Power Facility: –Full capacity: 72 MW • Both Gariep and Vanderkloof supply electricity during peak demand and emergency periods (peaking stations), through the Eskom national Great Karoo, Karoo also spelled Karroo, Afrikaans Groot Karoo, also called Central Karoo, plateau basin in Western Cape province, South Africa, lying between the Great Escarpment (north) and the Swartberg (south). Memoirs 36:223–231, Frimmel HE, Board WS (2000) Fluid evolution in and around the Rosh Pinah massive sulphide deposit in the external Pan-African Gariep Belt, Namibia. Tectonophysics 375:261–288, Middlemost EAK (1963) Geology of the southeastern Richtersveld. Mem Geol Surv S Afr 79:1–163, Gresse PG (1994) Strain partitioning in the southern Gariep Arc as reflected by sheath folds and stretching lineations. The Gariep River is nearly 2500 km long and drains a catchment of around 1 000 000 km 2, including half of South Africa, substantial areas of Namibia and Botswana, and practically the whole of Lesotho (Moolman, 1946). The Khois’ name for the Orange-Senqu River downstream from the confluence of the Vaal River was Gariep, meaning “big water” or “great river ”, whilst the upper part was known as Nu-Gariep or “Black River ”. J Afr Earth Sci 21:9–33, Halverson GP et al (2005) Towards a Neoproterozoic composite carbon isotope record. Precambrian Research Unit, University of Cape Town. The wall is 88 m high and has a crest length of 914 m and contains approximately 1.73 million m³ of concrete. Memoirs, vol 36, pp 195–209, Hoffman PF, Schrag DP (2002) The snowball Earth hypothesis: testing the limits of global change. CONTEXT 1 2.1 General Context 1 2.2 An IWRM Plan for the Orange-Senqu Basin 3 3. Figure 2.33 Landtypes of the Gariep basin as defined by the Institute for Soil, Climate and Water, Agricultural Research Council. basin translate: 容器, 盆；水盆, 一盆（的量）, 洗手池；洗脸盆, 区域, 流域, 船坞；内湾. Trans Geol Soc S Afr 86:293–299, Will T et al (2014) Geochemical and isotope evidence for initiation of Cretaceous South Atlantic opening along a former Neoproterozoic back-arc basin: implications for the location of the main Pan-African suture in southwest Gondwana. Hydrology. Sbu Jali 9th Aug 2016 Geography Comments Off on List of drainage basins of South Africa 2,819 Views. Precambrian Res 185:149–163, Lohmeyer M (2013) Methodische Entwicklung GIS-basierter geogener Rohstoffpotentialkarten am Beispiel des südwestlichen Namibia. (unused due to lack of maintenance). Geology 44:955–958, Ransome IGD (1992) The geochemistry, kinematics and geodynamics of the Gannakouriep dyke swarm. 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