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Dune 7 (Namibia)
Dune 7 is the highest dune in Namibia. The dune has been measured at over 1,256 feet (383 meters) and is named Dune 7 because it is the seventh dune one encounters after crossing the river Tsauchab 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 .... References Dunes of Namibia Walvis Bay {{Namibia-geo-stub ...
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Duna 7, Walvis Bay, Namibia, 2018-08-05, DD 15-17 PAN
Duna is the Hungarian name for the Danube River. Other places with the name Duna include: *D'Una River, Brazil *Duna (woreda), Hadiya Zone, Ethiopia *Duna, Iran (other), places in Iran * 23617 Duna, main-belt asteroid discovered in 1996 Duna may also refer to: *Duna TV, Hungarian television station *Duna World, Hungarian television station and sister channel of Duna TV *Duna or Dyna, the Viking name, or Düna, the German name for the Daugava (river) (flowing through Russia, Belarus, and Latvia) *Duna (band), Soviet band of the late 1980s *Duna Records, American record label founded by Brant Bjork *Fiat Duna, small car produced in Brazil *Duna language, spoken in Papua New Guinea *Duna people, indigenous people living in Papua New Guinea People with the given name or surname Duna include: * Steffi Duna, Hungarian actress See also *Doona, Australian term for duvet A duvet (, ; ), usually called a comforter or (''down-filled'') quilt in US English, and a doona in Aus ...
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Dune
A dune is a landform composed of wind- or water-driven sand. It typically takes the form of a mound, ridge, or hill. An area with dunes is called a dune system or a dune complex. A large dune complex is called a dune field, while broad, flat regions covered with wind-swept sand or dunes with little or no vegetation are called '' ergs'' or ''sand seas''. Dunes occur in different shapes and sizes, but most kinds of dunes are longer on the stoss (upflow) side, where the sand is pushed up the dune, and have a shorter ''slip face'' in the lee side. The valley or trough between dunes is called a ''dune slack''. Dunes are most common in desert environments, where the lack of moisture hinders the growth of vegetation that would otherwise interfere with the development of dunes. However, sand deposits are not restricted to deserts, and dunes are also found along sea shores, along streams in semiarid climates, in areas of glacial outwash, and in other areas where poorly cemented s ...
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Tsauchab
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. The Tsauchab is approximately long, its catchment area (including its tributary, the Zebra River) is estimated to be between 4,000 and . Since it is in the Namib Desert, the Tsauchab carries water only during the rare times when rain falls in the Naukluft Mountains and runs off, since it cannot seep into the soil fast enough (see ''flash flood''). During these rains, the Tsauchab becomes a rapid-running, strong river within a matter of hours. As a result of the occasional rains, it has over the past two million years carved the Sesriem Canyon, a long and up to deep canyon in sedimentary rock. Past the canyon, the ...
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Dunes Of Namibia
A dune is a landform composed of wind- or water-driven sand. It typically takes the form of a mound, ridge, or hill. An area with dunes is called a dune system or a dune complex. A large dune complex is called a dune field, while broad, flat regions covered with wind-swept sand or dunes with little or no vegetation are called '' ergs'' or ''sand seas''. Dunes occur in different shapes and sizes, but most kinds of dunes are longer on the stoss (upflow) side, where the sand is pushed up the dune, and have a shorter ''slip face'' in the lee side. The valley or trough between dunes is called a ''dune slack''. Dunes are most common in desert environments, where the lack of moisture hinders the growth of vegetation that would otherwise interfere with the development of dunes. However, sand deposits are not restricted to deserts, and dunes are also found along sea shores, along streams in semiarid climates, in areas of glacial outwash, and in other areas where poorly cemented sa ...
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