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Kombat (the place of the giraffe [citation needed]) is a mine and its associated settlement at the southern margin of the Otavi Mountain Range in northern Namibia. It is situated 37 kilometres (23 mi) East of Otavi on the B8 to Grootfontein. [1] Kombat at its peak had over 1,000 inhabitants.
Crossing the Trans–Caprivi Highway on approach to Katima's Mpacha Airport.. B8 road often known as the Golden Highway [1] is one of the national highways of Namibia.It leads from the B1 at Otavi via Grootfontein and Rundu through the Caprivi Strip to the border town of Katima Mulilo (where there is a short 4-kilometre (2.5 mi) spur section, also designated B8, crossing into Zambia) and ...
The problem entails finding such a place in the world ocean where, if a person fell overboard while on a ship at sea, they would be as far away from any land in any direction as possible. It lies in the South Pacific Ocean , and is equally distant from the three closest land vertices which are each roughly 2,688 km (1,670 mi) away.
Elefantenberg south of Otavi next to the B1 (2014) Otavi is a railway junction where the line from Windhoek to Oshikango branches off the line to Grootfontein. The town is served by the Otavi railway station. Otavi is situated next to the B1 - the longest National Road, running the length of Namibia - about 370 km from the capital, Windhoek.
The Strait of Gibraltar [1] is a narrow strait that connects the Atlantic Ocean to the Mediterranean Sea and separates Europe from Africa.The two continents are separated by 7.7 nautical miles (14.2 kilometers, 8.9 miles) at its narrowest point. [2]
The proposal for the name Southern Ocean won 18 votes, beating the alternative Antarctic Ocean. Half of the votes supported a definition of the ocean's northern limit at 60°S (with no land interruptions at this latitude), with the other 14 votes cast for other definitions, mostly 50°S, but a few for as far north as 35°S.
The deposition of the Nosib Formation (900-750 Ma) is the original deposition from the mass wasting of the newly uplifted edges of the Congo Craton, followed by the Otavi Formation (750-650 Ma), composed of dolomite and limestone from the formation of the shallow sea. [1]
The Firth of Clyde merges with the channel, between the southern tip of the Kintyre peninsula and Corsewall Point on the Rhins of Galloway. [2] The channel begins north of the Isle of Man and is customarily considered part of the Irish Sea, the channel runs north-west into the Atlantic Ocean. [3]
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