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Kibara Mountains
The Kibara Mountains (French: Monts Kibara) are a range in the Katanga Province of the Democratic Republic of the Congo. They are partly within the Upemba National Park. The Kibara mountains were once part of a continuous plateau in northern Katanga that also included the Mitumba and Kundelungu blocks, and has now been divided by deep valleys. The Upemba depression lies to the west of the Kibara mountains. The Lufira River separates them from the Mitumba Mountains to the east. The Kibara mountains have an average elevation of above sea level and a highest elevation of . Above the soil is generally poor, sandy and partly lateritized, and becomes very dry in the dry season. Vegetation is low grassland or steppe. There are few trees or bushes. The mountains have a NE-SW trend, and are folded and intruded. They have been strongly uplifted. The fragmented surface from the end of the Cretaceous at Lumbele occurs at an elevation of , above the Mid-Cenozoic pediplain at Mkana at an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Katanga Province
Katanga was one of the four large provinces created in the Belgian Congo in 1914. It was one of the eleven provinces of the Democratic Republic of the Congo between 1966 and 2015, when it was split into the Tanganyika Province, Tanganyika, Haut-Lomami, Lualaba Province, Lualaba, and Haut-Katanga provinces. Between 1971 and 1997 (during the rule of Mobutu Sese Seko when Congo was known as Zaire), its official name was Shaba Province. Katanga's area encompassed . Farming and ranching are carried out on the Katanga Plateau. The eastern part of the province is considered to be a rich mining region, which supplies cobalt, copper, tin, radium, uranium, and diamonds. The region's former capital, Lubumbashi, is the second-largest city in the Congo. History Copper mining in Katanga dates back over 1,000 years, and mines in the region were producing standard-sized ingots of copper for international transport by the end of the 10th century CE. In the 1890s, the province was beleaguered ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Democratic Republic Of The Congo
The Democratic Republic of the Congo (french: République démocratique du Congo (RDC), colloquially "La RDC" ), informally Congo-Kinshasa, DR Congo, the DRC, the DROC, or the Congo, and formerly and also colloquially Zaire, is a country in Central Africa. It is bordered to the northwest by the Republic of the Congo, to the north by the Central African Republic, to the northeast by South Sudan, to the east by Uganda, Rwanda, and Burundi, and by Tanzania (across Lake Tanganyika), to the south and southeast by Zambia, to the southwest by Angola, and to the west by the South Atlantic Ocean and the Cabinda exclave of Angola. By area, it is the second-largest country in Africa and the 11th-largest in the world. With a population of around 108 million, the Democratic Republic of the Congo is the most populous officially Francophone country in the world. The national capital and largest city is Kinshasa, which is also the nation's economic center. Centered on the Cong ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upemba National Park
Upemba National Park is a large national park in Haut-Lomami, Lualaba Province & Haut-Katanga Province (formerly in Katanga Province) of the southeastern Democratic Republic of Congo, formerly Zaire. Geography At the time of the creation of Upemba National Park, on 15 May 1939, the park had a surface area of . It was the largest park in Africa. In July 1975, the limits were revised and today the integral park has an area of with an annex of a further . Its lower section is located in the Upemba Depression, a lush area of lakes and marshes including the eponymous Lake Upemba, and bordered by the Lualaba River. Its higher section is in the dryer Kibara Plateau mountains. History Upemba National Park was first established in 1939. As with much of the wildlife of the region, in contemporary times the park continues to be threatened by the activities of poachers, pollution, and the activities of refugees and militia. There are also a handful of villages in the park. In recent yea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lufira River
The Lufira River is a tributary of the Lualaba River in the Democratic Republic of the Congo (DRC). The Lufira rises in the Shaba plateau south of Likasi. The river was dammed in 1926 at Mwadingusha near Likasi to form Lake Tshangalele, a reservoir for a hydroelectric generator supplying power for copper smelting. It flows northwards through the Bia Mountains for about , joining the Lualaba in Lake Kisale Lake Kisale is a lake in the Democratic Republic of the Congo (DRC), in Bukama Territory, Haut-Lomami District. At about in area, it is the second largest of the lakes in the Upemba Depression (Kamolondo Depression), an extensive marshy area part .... References Lualaba River Rivers of the Democratic Republic of the Congo Ramsar sites in the Democratic Republic of the Congo {{DRCongo-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cenozoic
The Cenozoic ( ; ) is Earth's current geological era, representing the last 66million years of Earth's history. It is characterised by the dominance of mammals, birds and flowering plants, a cooling and drying climate, and the current configuration of continents. It is the latest of three geological eras since complex life evolved, preceded by the Mesozoic and Paleozoic. It started with the Cretaceous–Paleogene extinction event, when many species, including the non-avian dinosaurs, became extinct in an event attributed by most experts to the impact of a large asteroid or other celestial body, the Chicxulub impactor. The Cenozoic is also known as the Age of Mammals because the terrestrial animals that dominated both hemispheres were mammalsthe eutherians (placentals) in the northern hemisphere and the metatherians (marsupials, now mainly restricted to Australia) in the southern hemisphere. The extinction of many groups allowed mammals and birds to greatly diversify so that l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kibaran Orogeny
The Kibaran orogeny is a term that has been used for a series of orogenic events, in what is now Africa, that began in the Mesoproterozoic, around 1400 Ma and continued until around 1000 Ma when the supercontinent Rodinia was assembled. The term "Kibaran" has often been used for any orogenic rocks formed during this very extended period. Recently, it has been proposed that the term should be used in a much narrower sense for an event around 1375 Ma and a region in the southeast of the Democratic Republic of the Congo (DRC). These orogenic events are also known as the Grenville orogeny in North America and the Dalslandian orogeny in Western Europe. Broad sense Regions that contain relics of Kibaran age include the Kibara Mountains of the eastern DRC and Namaqua-Natal belt in southern Africa. Rocks of this age have been found in the Hoggar Mountains, in northwest and southwest Nigeria and in Cameroon to the north of the Congo Craton. The orogeny in northwest Nigeria was a major t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geosyncline
A geosyncline (originally called a geosynclinal) is an obsolete geological concept to explain orogens, which was developed in the late 19th and early 20th centuries, before the theory of plate tectonics was envisaged. Şengör (1982), p. 11 A geosyncline was described as a giant downward fold in the Earth's crust, with associated upward folds called geanticlines (or geanticlinals), that preceded the climax phase of orogenic deformation. History The geosyncline concept was first conceived by the American geologists James Hall and James Dwight Dana in the mid-19th century, during the classic studies of the Appalachian Mountains. Émile Haug further developed the geosyncline concept, and introduced it to Europe in 1900. Şengör (1982), p. 26 Eduard Suess, a leading geologist of his time, disapproved the concept of geosyncline, and in 1909 he argued against its use due to its association with outdated theories. Şengör (1982), p. 43 This did not prevent further development of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of The Democratic Republic Of The Congo
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 300 metres (1,000 feet) 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haut-Katanga Province
Haut-Katanga (French for "Upper Katanga") is one of the 21 new provinces of the Democratic Republic of the Congo created in the 2015 repartitioning. Haut-Katanga, Haut-Lomami, Lualaba, and Tanganyika provinces are the result of the dismemberment of the former Katanga province. Haut-Katanga was formed from the Haut-Katanga district and the independently administered cities of Likasi and Lubumbashi. Lubumbashi retained its status as a provincial capital. The new province's territory corresponds to the historic Katanga-Oriental that existed in the early period after independence between 1963 and 1966. Territories Its current territories are: * Kasenga * Kipushi * Mitwaba * Pweto * Sakania Sakania is a town in Haut-Katanga Province, in the Congo Pedicle, in the far south of the Democratic Republic of Congo, near the border with Zambia. It is located at an elevation of 1278m asl, therefore it has a cool climate. Between 1935 and 1939 i ... Approximate correspondence between ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
