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Demarcation of Water Basins on National Level - EIS

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Basin <str<strong>on</strong>g>Demarcati<strong>on</strong></str<strong>on</strong>g><br />

4.2 OKAVANGO-OMATAKO BASIN<br />

The Okavango-Omatako Basin comprises as menti<strong>on</strong>ed above some <str<strong>on</strong>g>of</str<strong>on</strong>g> the most important surface and<br />

groundwater resources in Namibia. The Okavango River <strong>on</strong> the border to Angola is tapped for<br />

irrigati<strong>on</strong> projects al<strong>on</strong>g the river and a planned bulk water pipeline from Rundu to Grootf<strong>on</strong>tein<br />

would secure the sustainable water supply to the central area. The groundwater resources in the<br />

Grootf<strong>on</strong>tein Karst Area, represent the most productive aquifers in Namibia and are c<strong>on</strong>sidered a<br />

strategic reserve and emergency source in case the main water supply dams <str<strong>on</strong>g>of</str<strong>on</strong>g> central area fall dry.<br />

The Grootf<strong>on</strong>tein Karst Area is c<strong>on</strong>nected to the central area by the Eastern <str<strong>on</strong>g>Water</str<strong>on</strong>g> Carrier, which<br />

allow the gravity flow <str<strong>on</strong>g>of</str<strong>on</strong>g> the groundwater to the Omatako Dam and from there to the V<strong>on</strong> Bach Dam<br />

at Okahandja.<br />

The above bulk water supply projects are partly opposed by farmers in the Karst Area, who are afraid<br />

<str<strong>on</strong>g>of</str<strong>on</strong>g> groundwater mining and over abstracti<strong>on</strong> with negative effect <strong>on</strong> the local groundwater table and<br />

pumping costs. The abstracti<strong>on</strong> from the Okavango River is <str<strong>on</strong>g>of</str<strong>on</strong>g> internati<strong>on</strong>al c<strong>on</strong>cern because <str<strong>on</strong>g>of</str<strong>on</strong>g> the<br />

possible influence <strong>on</strong> the Okavango Delta. The Okavango-Omatako Basin has like the Swakop-<br />

Omaruru Basin high priority regarding a water basin pr<str<strong>on</strong>g>of</str<strong>on</strong>g>ile. An inaugurati<strong>on</strong> meeting should be<br />

organized and held in Rundu.<br />

4.3 ORANGE-FISH BASIN<br />

The perennial Orange River is the most important water source <str<strong>on</strong>g>of</str<strong>on</strong>g> southern Namibia, an area that is<br />

known for arid climatic c<strong>on</strong>diti<strong>on</strong>s and water scarcity. The river water is utilized for large-scale<br />

agricultural irrigati<strong>on</strong> projects and for mining operati<strong>on</strong>s. The ec<strong>on</strong>omically very important base metal<br />

mines at Rosh Pina and Scorpi<strong>on</strong> are supplied with fresh water via a bulk pipeline, operated by<br />

Nam<str<strong>on</strong>g>Water</str<strong>on</strong>g>. The ephemeral Fish River is a tributary to the Orange River and feeds the largest dam in<br />

Namibia, the Hardap Dam. The water is used for the water supply to Mariental but mainly for<br />

irrigati<strong>on</strong> projects in the surroundings. A tributary to the Fish River recharges the Naute Dam, south <str<strong>on</strong>g>of</str<strong>on</strong>g><br />

Keetmanshoop. The water <str<strong>on</strong>g>of</str<strong>on</strong>g> this dam is also used mainly for agricultural projects.<br />

The above bulk water sources are <str<strong>on</strong>g>of</str<strong>on</strong>g> great importance for the development <str<strong>on</strong>g>of</str<strong>on</strong>g> the sparsely populated<br />

but ec<strong>on</strong>omically increasingly important southern part <str<strong>on</strong>g>of</str<strong>on</strong>g> Namibia. Future possible developments<br />

include a gas power stati<strong>on</strong> at Oranjemund, additi<strong>on</strong>al irrigati<strong>on</strong> projects al<strong>on</strong>g the Orange River, a<br />

possible joint Namibian/South African Orange River Dam, and additi<strong>on</strong>al dams al<strong>on</strong>g the Fish River<br />

downstream the Hardap Dam. All these planned activities will have and effect <strong>on</strong> the envir<strong>on</strong>mental<br />

and socio-ec<strong>on</strong>omic situati<strong>on</strong> and the decisi<strong>on</strong>-making will have to be d<strong>on</strong>e in close co-laborati<strong>on</strong> with<br />

the proposed basin management committee. An inaugurating meeting should be held at Oranjemund.<br />

4.4 ZAMBESI-KWANDO-LINYANTI BASIN<br />

The Zambesi, Kwando and Linyanti-Chobe rivers surround the Caprivi Regi<strong>on</strong> in the east, west and<br />

south. The populati<strong>on</strong> density is highest al<strong>on</strong>g the river courses because <str<strong>on</strong>g>of</str<strong>on</strong>g> the abundance <str<strong>on</strong>g>of</str<strong>on</strong>g> fresh<br />

water. The interior <str<strong>on</strong>g>of</str<strong>on</strong>g> the Caprivi regi<strong>on</strong> is <str<strong>on</strong>g>of</str<strong>on</strong>g>ten characterized by saline groundwater c<strong>on</strong>diti<strong>on</strong>s and<br />

because <str<strong>on</strong>g>of</str<strong>on</strong>g> this, large areas are under-developed. Recent groundwater explorati<strong>on</strong> studies have shown<br />

that this saline water is underlain by deeper freshwater and future development would include the<br />

sustainable exploitati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> the newly detected source. Groundwater is a cost effective alternative to<br />

pipeline water from the rivers and should be encouraged through the proposed basin management<br />

committee.<br />

Bittner <str<strong>on</strong>g>Water</str<strong>on</strong>g> C<strong>on</strong>sult 2004 GTZ, MAWRD<br />

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