Caledon (river)
Caledon mohokare |
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An old map of Lesoto's, with the Caledon as the border river (above) |
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Data | ||
location |
South Africa Lesotho |
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River system | Orange | |
Drain over | Orange → Atlantic | |
source | near the place Libono | |
Source height | about 2700 m | |
muzzle | at Bethulie in the Orange Coordinates: 30 ° 31 ′ 22 " S , 26 ° 4 ′ 4" E 30 ° 31 ′ 22 " S , 26 ° 4 ′ 4" E |
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Mouth height | 1261 m | |
Height difference | about 1439 m | |
Bottom slope | about 3 ‰ | |
length | 480 km | |
Catchment area | 15,266 km² | |
Discharge at gauge D2H022 A Eo : 12,952 km² |
MNQ 1988-2009 MQ 1988-2009 Mq 1988-2009 MHQ 1988-2009 |
11 m³ / s 34 m³ / s 2.6 l / (s km²) 69 m³ / s |
Reservoirs flowed through | Gariep Reservoir , Welbedacht Reservoir | |
Big cities | Maseru | |
The Caledon or Mohokare , as it is also called in Lesotho, is a right tributary of the Orange River in South Africa .
course
It flows preferentially in a south-westerly direction and forms the north-western border of Lesotho . It rises near the place Libono , almost at the northernmost point of Lesotho at an altitude of around 2700 m. There is a second, larger source river, which rises to the north and is called Little Caledon .
The capital of Lesotho, Maseru , is on the Caledon, as is the South African city of Ficksburg further north .
Dams
About 30 km southwest of Wepener , the Caledon is dammed by the Welbedacht reservoir . The Caledon flows into the Oranje at Bethulie and feeds the Gariep reservoir with it . The Caledon is rich in sediments , which leads to problems in the reservoirs, as they quickly lose their storage capacity.
Hydrometry
The flow rate of the Caledon was measured in m³ / s at a station shortly before the mouth, at around 85% of the catchment area (1988 to 2009, values read from the diagram).
Individual evidence
- ↑ Caledon River ( English ) In: Encyclopædia Britannica . Retrieved January 16, 2009.
- ^ A b c Water Resources Availability in the Caledon River Basin Past, Present and Future