Höchster Porzellanmanufaktur
   HOME





Höchster Porzellanmanufaktur
Höchster ("The Highest") is a mountain in the Diamond Restricted Area, also called ''Sperrgebiet'', in the southwestern part of Namibia. It reaches a height of 1,070 m. Its expansion is about 5 km × 4 km. West of ''Höchster'' are the Klinghardt Mountains. Several places of the mountain range are covered with sand which is blown over by sandstorms. The average yearly rainfall in this area of the Namib amounts to just a few millimeters.Fog desert Namib The bushes to be found in the mountains just survive because of the mist, which sometimes is formed above the cold Atlantic and then during daytime drifts far into the desert. The few Camel Thorn trees take their water from deep underground accumulations.Camel Thorn Camelthorn or camel thorn is a common name for several plants and may refer to: *''Acacia erioloba'', a tree native to southern Africa *''Alhagi ''Alhagi'' is a genus of Old World plants in the family Fabaceae. They are commonly calle ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

ǁKaras Region
The ǁKharas Region (pronounced , with a lateral click, former name Karas Region, without the click) is the southernmost, largest, and least densely populated of the 14 regions of Namibia; its capital is Keetmanshoop. The name assigned to the region reflects the prominence of the Karas mountain range in its southern part. The ǁKharas region contains the municipality of Keetmanshoop, the towns Karasburg, Lüderitz and Oranjemund, and the self-governed villages Aroab, Berseba, Bethanie, Koës and Tses. ǁKharas' western border is the shores of the Atlantic Ocean. Its location in Namibia's south means that it shares a long border in the south and east with the Northern Cape Province of South Africa. Domestically, it borders only the Hardap Region, to the north. Politics As of 2020, ǁKharas had 56,352 registered voters. The name of this region was ''Karas Region'' (without the alveolar lateral click of the Khoekhoegowab language) since Namibian independence in 1990. I ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Namibia
Namibia, officially the Republic of Namibia, is a country on the west coast of Southern Africa. Its borders include the Atlantic Ocean to the west, Angola and Zambia to the north, Botswana to the east and South Africa to the south; in the northeast, approximating a quadripoint, Zimbabwe lies less than 200 metres (660 feet) away along the Zambezi, Zambezi River near Kazungula, Zambia. Namibia's capital and largest city is Windhoek. Namibia is the driest country in sub-Saharan Africa, and has been inhabited since prehistoric times by the Khoekhoe, Khoi, San people, San, Damara people, Damara and Nama people. Around the 14th century, immigration, immigrating Bantu peoples arrived as part of the Bantu expansion. From 1600 the Ovambo people#History, Ovambo formed kingdoms, such as Ondonga and Oukwanyama. In 1884, the German Empire established rule over most of the territory, forming a colony known as German South West Africa. Between 1904 and 1908, German troops waged a punitive ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Klinghardt Mountains
The Klinghardt Mountains are a Namibian mountain range in the Diamond Restricted Area, also called Sperrgebiet. The Klinghardt Mountains are located approximately 90 km south-southeast of Lüderitz and extend over an area of about 350 km2. East of the Klinghardt Mountains is the mountain Höchster. Several places of the mountain range are covered with sand which is blown over by sandstorms. The average yearly rainfall in this area of the Namib desert amounts to just a few millimeters.Fog desert Namib The bushes to be found in the mountains just survive because of the mist, which sometimes is formed above the cold Atlantic and then during daytime drifts far into the desert. The few Camel Thorn trees take their water from deep underground accumulations.Camel Thorn Camelthorn or camel thorn is a common name for several plants and may refer to: *''Acacia erioloba'', a tree native to southern Africa *''Alhagi ''Alhagi'' is a genus of Old World plants in the family ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Namib
The Namib ( ; ) is a coastal desert in Southern Africa. According to the broadest definition, the Namib stretches for more than along the Atlantic coasts of Angola, Namibia, and northwest South Africa, extending southward from the Carunjamba River in Angola, through Namibia and to the Olifants River (Western Cape), Olifants River in Western Cape, South Africa. The Namib's northernmost portion, which extends from the Angola-Namibia border, is known as Moçâmedes Desert, while its southern portion approaches the neighboring Kalahari Desert. From the Atlantic coast eastward, the Namib gradually ascends in elevation, reaching up to inland to the foot of the Great Escarpment, Southern Africa, Great Escarpment. Annual precipitation ranges from in the aridest regions to at the escarpment, making the Namib the only true desert in southern Africa. Having endured Desert climate, arid or Semi-arid climate, semi-arid conditions for roughly 55–80 million years, the Namib may be the old ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Fog Desert
A fog desert is a type of desert where fog drip supplies the majority of moisture needed by animal and plant life. Examples of fog deserts include the Atacama Desert of coastal Chile and Peru; the Baja California desert of Mexico; the Namib Desert in Namibia; the Arabian Peninsula coastal fog desert; and a manmade instance within Biosphere 2, an artificial closed ecosphere in Arizona. Formation Humidity in foggy air is above 95%. One way for fog to form in Desert, deserts is through the interaction of hot humid air (such as is formed above warm bodies of water) with a cooler object, such as a mountain. When warm air hits cooler objects, fog is generated by the condensation of vaporized water. Another way fog forms in deserts occurs when a desert is close to an ocean which has a cold current. When air is heated over desert land and blows towards the cool water in the ocean, it condenses and fog is formed. The cool fog is then blown inland by the ocean breeze. Fog is mainly for ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  




Vachellia Erioloba
''Vachellia erioloba'', the camel thorn, also known as the giraffe thorn, mokala tree, or Kameeldoring in Afrikaans, still more commonly known as ''Acacia erioloba'', is a tree of southern Africa in the family Fabaceae. Its preferred habitat is the deep dry sandy soils in parts of South Africa, Botswana, the western areas of Zimbabwe and Namibia. It is also native to Angola, south-west Mozambique, Zambia and Eswatini. The tree was first described by Ernst Heinrich Friedrich Meyer and Johann Franz Drège in 1836. The camel thorn is a protected tree in South Africa. The tree can grow up to 20 metres high. It is slow-growing, very hardy to drought and fairly frost-resistant. The light-grey colored thorns reflect sunlight, and the Pinnation, bipinnate leaves close when it is hot. The wood is dark reddish-brown in colour and extremely dense and strong. It is good for fires, which leads to widespread clearing of dead trees and the felling of healthy trees. It produces ear-shaped legume ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Höchster Sperrgebiet Luftaufnahme 2018
Höchster ("The Highest") is a mountain in the Sperrgebiet, Diamond Restricted Area, also called ''Sperrgebiet'', in the southwestern part of Namibia. It reaches a height of 1,070 m. Its expansion is about 5 km × 4 km. West of ''Höchster'' are the Klinghardt Mountains. Several places of the mountain range are covered with sand which is blown over by sandstorms. The average yearly rainfall in this area of the Namib amounts to just a few millimeters.Fog desert Namib The bushes to be found in the mountains just survive because of the mist, which sometimes is formed above the cold Atlantic and then during daytime drifts far into the desert. The few Vachellia erioloba, Camel Thorn trees take their water from deep underground accumulations.Vachellia erioloba, Camel Thorn trees have roots reaching 60 m in depth. References {{Commons category Mountains of Namibia Geography of ǁKaras Region ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Mountains Of Namibia
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains te ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]