Tsondab River | |
---|---|
Location | |
Physical characteristics | |
Source | Remhoogte Mountains |
⁃ location | Hardap Region |
Mouth | Tsondabvlei |
⁃ location | Hardap Region |
⁃ coordinates | 23°55′13″S15°22′11″E / 23.9203°S 15.3698°E Coordinates: 23°55′13″S15°22′11″E / 23.9203°S 15.3698°E |
Length | c.150 km (93 mi) |
Basin size | 3,500 km2 (1,400 sq mi) |
Basin features | |
Tributaries | |
⁃ left | Diep River |
⁃ right | Noab River, Koireb River |
The Tsondab River is an ephemeral river in the Hardap Region of central Namibia. Its source is in the Remhoogte Mountains. From there it flows westwards through the Namib-Naukluft National Park before evaporating at Tsondabvlei. Inflows of the Tsondab are Diep, Noab and Koireb. Tsondab's catchment area (including its tributaries) is 3,500 km2 (1,400 sq mi). [1] [2]
The Kuiseb River is an ephemeral river in western-central Namibia. Its source is in the Khomas Highland west of Windhoek. From there it flows westwards through the Namib-Naukluft National Park and the Namib desert to Walvis Bay. Several settlements of the Topnaar people are situated on the banks of the lower Kuiseb, for instance Homeb, Sandfontein, Rooibank, and Utuseb. Inflows of the Kuiseb are Gomab, Ojab, Chausib, Gaub, Koam, Nausgomab and Goagos.
The Ugab River is an ephemeral river in north-western Namibia. Its lower section forms the border between Kunene Region and Erongo Region but its catchment area extends well into the Otjozondjupa Region. Ugab's source is near Otavi. From there it the riverbed leads westwards past the Paresis Mountains and the Fransfontein Mountains into the Skeleton Coast and the Atlantic Ocean. Inflows of the Ugab are Erundu, Ozongombo, Okomize and Uis.
Outjo is a city of 6,000 inhabitants in the Kunene Region of Namibia. It is the district capital of Outjo Constituency. It is best known as a main gateway to Etosha National Park.
Uis is a settlement located in Erongo Region, Namibia. It belongs to the Dâures electoral constituency. Located in the former Damaraland, it is known for the local mineral wealth. The settlement was established in 1958 as workers' settlement to exploit local tin deposits. It has approximately 3,600 inhabitants and, before being downgraded from "village" to "settlement" in 2010, owned 10 square kilometres (3.9 sq mi) of land.
The Swakop River is a major river in western central Namibia. Its river source is in the Khomas Highland. From there it flows westwards through the town of Okahandja, the historic mission station at Gross Barmen, and the settlement of Otjimbingwe. It then crosses the Namib desert and reaches the Atlantic Ocean at Swakopmund. The Swakop is an ephemeral river; its run-off is roughly 40 million cubic metres per annum.
The Tsauchab is an ephemeral river in the Hardap Region of central Namibia. Its source is in the southern Naukluft Mountains, from where it flows westwards through the Namib-Naukluft National Park into Sossusvlei, an endorheic basin. The lower river has in the past had a slightly different courses and also formed two other basins, the Deadvlei and the Hiddenvlei.
Acanthosicyos horridus is an unusual melon that occurs in Namibia, South Africa, Angola and elsewhere; in English it is known as butter-nuts or butterpips, in one of the Khoisan languages it is locally called ǃnaras or ǃnara.
Twyfelfontein, officially known as ǀUi-ǁAis, is a site of ancient rock engravings in the Kunene Region of north-western Namibia. It consists of a spring in a valley flanked by the slopes of a sandstone table mountain that receives very little rainfall and has a wide range of diurnal temperatures.
The river Khan is an ephemeral river crossing the Erongo region of central Namibia. It is the main tributary of the Swakop River and only occasionally carries surface water during the rain seasons in November and February/March. Khan's catchment area including its tributaries Slang and Etiro is 8,400 square kilometres (3,200 sq mi).
The Annan River is a river located in the Wet Tropics of Far North Queensland, Australia.
The Omaruru River is a major river crossing the Erongo Region of western central Namibia from East to West. It originates in the Etjo Mountains, crosses the city of Omaruru and the village of Okombahe, and reaches the sea a few kilometers north of Henties Bay. Inflows of the Huab are Otjimakuru, Goab, Spitzkop, Leeu and Okandjou.
The Uniab River is an ephemeral river on Namibia's Skeleton Coast, located between Torra Bay and Terrace Bay. Its mouth is in the Grootberg Mountains near Palmwag. Inflows of the Uniab are Kaikams, Kawakab, Aub, Urenindes and Obob. The river once created a large river delta with five main watercourses. Today it continues to flow only in one of the watercourses, but subterranean water surfaces as springs in the other channels. Uniab's catchment area is estimated to be between 3961 and 4,500 km2 (1,700 sq mi).
The Hoanib is one of the 12 ephemeral seasonal rivers in the west of Namibia, where it was the border between northern Damaraland and Kaokoland. Its length is 270 km. With the low population density, the oasis character of the river valley and the relatively high wildlife population of Hoanib, together with the Hoarusib its valley is one of the last true wilderness areas in Namibia, one of the last settlements of desert elephants and shows strong wind and water eroded and weathered stone deposits. Inflows of Hoanib are Aap River, Otjitaimo River, Ombonde, Ganamub, Mudorib and Tsuxub.
The Ada River is a perennial river of the West Gippsland catchment, located in the West Gippsland region of the Australian state of Victoria.
Goreangab Dam is a dam in the north-western suburbs of Windhoek, the capital of Namibia. It dams the ephemeral Arebbusch River and its tributary, the Gammams River, which both run across Windhoek. The reservoir behind the dam has a capacity of 3.6 million cubic metres (4,700,000 cu yd).
The Hoarusib River is an ephemeral river in the Kunene Region region of north-western Namibia. Its source is near the regional capital Opuwo, and the river flows through the Tonnesen and Giraffe Mountains into the Atlantic Ocean. The Hoarusib occasionally carries surface water during the rainy seasons in November and February/March. The catchment area of the Hoarusib is 15,237 square kilometres (5,883 sq mi).
The river Khumib is an ephemeral river crossing the Kunene Region of north-western Namibia. It occasionally carries surface water during the rainy seasons in November and February/March. Its catchment area is estimated between 2200 and 2,300 square kilometres (890 sq mi).
The Koigab River is an ephemeral river on Namibia's Skeleton Coast. Its mouth is in the Grootberg Mountains near Bergsig, where its two inflows, the Gui-Tsawisib and the Springbok are located. Koigab's catchment area is estimated to be between 2320 and 2,400 km2 (930 sq mi).
The Huab River is an ephemeral river in the Kunene Region of north-western Namibia. Its source is southeast of Kamanjab, from where it flows westwards through Mopane savanna until it reaches the Skeleton Coast and the Atlantic Ocean. Inflows of the Huab are Klein Omaruru, Sout, Aba Huab, Ongwati and Klip. Uniab's catchment area is estimated to be between 14,800 and 16,465 km2 (6,357 sq mi), and includes the town of Khorixas as well as the settlements Kamanjab, Fransfontein, and Anker. The Twyfelfontein World Heritage Site is located on the banks of the Aba Huab.
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