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Mukurob
The Mukurob, also Mukorob, (Finger of God) near Asab in Namibia, was a sandstone rock formation in the Namib desert which collapsed on 7 December 1988. Geology Mukurob consisted mostly of sandstone. The structure was 12 m high and up to 4.5 m wide, and weighed some 450 tons. What made Mukorob so special, however, was its base. Just 3 m long and 1.5 m wide, it was much narrower than the mass of rock which it supported. Mukurob was once part of the Weissrand Plateau before 50,000 years of erosion slowly isolated the structure from the rest of the plateau. History Early history Mukurob was known to the Nama people for generations and inspired many tales and legends; this legend explains the structure's name and was told in many versions: "The Herero people had been at odds with the Nama people since time immemorial. One day a large group of Herero and their well-fed cattle came from the grazing areas in central Namibia to the Nama region in the arid south. “Look here, how rich ...
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Mukurob
The Mukurob, also Mukorob, (Finger of God) near Asab in Namibia, was a sandstone rock formation in the Namib desert which collapsed on 7 December 1988. Geology Mukurob consisted mostly of sandstone. The structure was 12 m high and up to 4.5 m wide, and weighed some 450 tons. What made Mukorob so special, however, was its base. Just 3 m long and 1.5 m wide, it was much narrower than the mass of rock which it supported. Mukurob was once part of the Weissrand Plateau before 50,000 years of erosion slowly isolated the structure from the rest of the plateau. History Early history Mukurob was known to the Nama people for generations and inspired many tales and legends; this legend explains the structure's name and was told in many versions: "The Herero people had been at odds with the Nama people since time immemorial. One day a large group of Herero and their well-fed cattle came from the grazing areas in central Namibia to the Nama region in the arid south. “Look here, how rich ...
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Asab
Asab ( Nama: ''new thing'') is a settlement in the ǁKaras Region of southern Namibia. It is situated on the B1 national road about halfway between Mariental and Keetmanshoop. east of Asab is the Mukurob rock pinnacle, a tourist attraction that collapsed in 1988. Asab belongs to the Berseba electoral constituency. The settlement features a petrol station, a shop, and a small hotel, although none of these businesses is operational, to the effect that the place has been described as a "ghost village". Asab Railway Station is a stop on the TransNamib railway line from Windhoek to Keetmanshoop. outside Asab there is the community of Groendoring (literally af, Green Thorn, referring to the Torchwood ''Torchwood'' is a British science fiction television programme created by Russell T Davies. A spin-off of the 2005 revival of ''Doctor Who'', it aired from 2006 to 2011. The show shifted its broadcast channel each series to reflect its growing ... of the Balanites genus), w ...
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Namibia Mukurob 01
Namibia (, ), officially the Republic of Namibia, is a country in Southern Africa. Its western border is the Atlantic Ocean. It shares land borders with Zambia and Angola to the north, Botswana to the east and South Africa to the south and east. Although it does not border Zimbabwe, less than 200 metres (660 feet) of the Botswanan right bank of the Zambezi River separates the two countries. Namibia gained independence from South Africa on 21 March 1990, following the Namibian War of Independence. Its capital and largest city is Windhoek. Namibia is a member state of the United Nations (UN), the Southern African Development Community (SADC), the African Union (AU) and the Commonwealth of Nations. The driest country in sub-Saharan Africa, Namibia has been inhabited since pre-historic times by the San, Damara and Nama people. Around the 14th century, immigrating Bantu peoples arrived as part of the Bantu expansion. Since then, the Bantu groups, the largest being the Ovambo, ha ...
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Namibia
Namibia (, ), officially the Republic of Namibia, is a country in Southern Africa. Its western border is the Atlantic Ocean. It shares land borders with Zambia and Angola to the north, Botswana to the east and South Africa to the south and east. Although Kazungula, it does not border Zimbabwe, less than 200 metres (660 feet) of the Botswanan right bank of the Zambezi, Zambezi River separates the two countries. Namibia gained independence from South Africa on 21 March 1990, following the Namibian War of Independence. Its capital and largest city is Windhoek. Namibia is a member state of the United Nations (UN), the Southern African Development Community (SADC), the African Union (AU) and the Commonwealth of Nations. The driest country in sub-Saharan Africa, Namibia has been inhabited since pre-historic times by the San people, San, Damara people, Damara and Nama people. Around the 14th century, immigration, immigrating Bantu peoples arrived as part of the Bantu expansion. Since ...
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Namib
The Namib ( ; pt, Namibe) is a coastal desert in Southern Africa. The name is of Khoekhoegowab origin and means "vast place". According to the broadest definition, the Namib stretches for more than along the Atlantic coasts of Angola, Namibia, and South Africa, extending southward from the Carunjamba River in Angola, through Namibia and to the 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. Annual precipitation ranges from in the most arid regions to at the escarpment, making the Namib the only true desert in southern Africa. Having endured arid or semi-arid conditions for roughly 55–80 million years, the Namib may be the oldest desert in the world and conta ...
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Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ...
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Nama People
Nama (in older sources also called Namaqua) are an African ethnic group of South Africa, Namibia and Botswana. They traditionally speak the Nama language of the Khoe-Kwadi language family, although many Nama also speak Afrikaans. The Nama People (or Nama-Khoe people) are the largest group of the Khoikhoi people, most of whom have disappeared as a group, except for the Namas. Many of the Nama clans live in Central Namibia and the other smaller groups live in Namaqualand, which today straddles the Namibian border with South Africa. History For thousands of years, the Khoisan peoples of South Africa and southern Namibia maintained a nomadic life, the Khoikhoi as pastoralists and the San people as hunter-gatherers. The Nama are a Khoikhoi group. The Nama originally lived around the Orange River in southern Namibia and northern South Africa. The early colonialists referred to them as Hottentots. Their alternative historical name, "Namaqua", stems from the addition of the Khoekhoe ...
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Herero People
The Herero ( hz, Ovaherero) are a Bantu ethnic group inhabiting parts of Southern Africa. There were an estimated 250,000 Herero people in Namibia in 2013. They speak Otjiherero, a Bantu language. Though the Herero primarily reside in Namibia, there are also significant populations in Botswana and Angola. In Botswana, the Hereros or Ovaherero are mostly found in Maun and some villages surrounding Maun. These villages among others are Sepopa, Toromuja, Karee and Etsha. Some of them are at Mahalapye. In the South eastern part of Botswana they are at Pilane. There are also a few of them in the Kgalagadi South, that is Tsabong, Omawaneni, Draaihoek and Makopong Villages. Overview Unlike most Bantu, who are primarily subsistence farmers,Immaculate N. Kizza, ''The Oral Tradition of the Baganda of Uganda: A Study and Anthology of Legends, Myths, Epigrams and Folktales'' p. 21: "The Bantu were, and still are, primarily subsistence farmers who would settle in areas, clear land, or ...
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South West Africa
South West Africa ( af, Suidwes-Afrika; german: Südwestafrika; nl, Zuidwest-Afrika) was a territory under South African administration from 1915 to 1990, after which it became modern-day Namibia. It bordered Angola (Portuguese colony before 1975), Botswana ( Bechuanaland before 1966), South Africa, and Zambia (Northern Rhodesia before 1964). Previously the German colony of South West Africa from 1884–1915, it was made a League of Nations mandate of the Union of South Africa following Germany's defeat in the First World War. Although the mandate was abolished by the United Nations in 1966, South African control over the territory continued despite its illegality under international law. The territory was administered directly by the South African government from 1915 to 1978, when the Turnhalle Constitutional Conference laid the groundwork for semi-autonomous rule. During an interim period between 1978 and 1985, South Africa gradually granted South West Africa a limited for ...
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Spitak Earthquake
The 1988 Armenian earthquake, also known as the Spitak earthquake ( hy, Սպիտակի երկրաշարժ, ), occurred on December 7 at with a surface wave magnitude of 6.8 and a maximum MSK intensity of X (''Devastating''). The shock occurred in the northern region of Armenia (then part of the Soviet Union) which is vulnerable to large and destructive earthquakes and is part of a larger active seismic belt that stretches from the Alps to the Himalayas. Activity in the area is associated with tectonic plate boundary interaction and the source of the event was slip on a thrust fault just to the north of Spitak. The complex incident ruptured multiple faults, with a strike-slip event occurring shortly after the initiation of the mainshock. Between 25,000 and 50,000 were killed and up to 130,000 were injured. Seismologists thoroughly studied the effects of the Spitak event, including the mainshock and aftershock fault rupture mechanisms, and were on site setting up temporary seis ...
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