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Mount Marsabit
Marsabit is a 6300 km basaltic shield volcano in Kenya, located 170 km east of the center of the East African Rift, in Marsabit County near the town of Marsabit. This was primarily built during the Miocene, but some lava flows and explosive maar-forming eruptions have occurred more recently. At least two of the maars host crater lakes. The volcano is covered by dense forest. Marsabit National Park is in the area. It was here, near a body of water they dubbed Lake Paradise, that American explorers Martin and Osa Johnson spent time in the 1920s living and making wildlife documentaries. See also * List of volcanoes in Kenya This is a short list of active and extinct volcanoes in Kenya.For a more comprehensive list of volcanoes and craters in Kenya, see :sw:Orodha ya volkeno nchini Kenya List of volcanoes in Kenya (non-exhaustive) References * Volcanoes of ... References External links * https://web.archive.org/web/20051224155242/http://www.kenyaforests. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Province (Kenya)
The Eastern Province ( sw, Mashariki) of Kenya was one of 8 Provinces of Kenya. Its northern boundary ran along with that of Ethiopia; the North Eastern Province and Coast Province lay to the east and south; and the remainder of Kenya's provinces, including Central Province, ran along its western border. The provincial capital was Embu. Overview On 16 July 2009, the province was sub-divided into 3 Sub-Provinces namely lower eastern with Machakos as headquarters, central eastern with Meru as headquarters, and upper eastern with Marsabit as headquarters; however those changes never took effect due to the political wrangles in the Kenyan coalition government at the time. The sub-division of provinces were carried out in all seven Provinces of Kenya, excluding Nairobi. As of March 2013 after the Kenyan general election, 2013, the Eastern Province was subdivided into 8 counties namely: The province was principally inhabited by the Meru, Kamba and Embu and several pastoralis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kenya
) , national_anthem = "Ee Mungu Nguvu Yetu"() , image_map = , map_caption = , image_map2 = , capital = Nairobi , coordinates = , largest_city = Nairobi , official_languages = Constitution (2009) Art. 7 ational, official and other languages"(1) The national language of the Republic is Swahili. (2) The official languages of the Republic are Swahili and English. (3) The State shall–-–- (a) promote and protect the diversity of language of the people of Kenya; and (b) promote the development and use of indigenous languages, Kenyan Sign language, Braille and other communication formats and technologies accessible to persons with disabilities." , languages_type = National language , languages = Swahili , ethnic_groups = , ethnic_groups_year = 2019 census , religion = , religion_year = 2019 census , demonym = ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shield Volcano
A shield volcano is a type of volcano named for its low profile, resembling a warrior's shield lying on the ground. It is formed by the eruption of highly fluid (low viscosity) lava, which travels farther and forms thinner flows than the more viscous lava erupted from a stratovolcano. Repeated eruptions result in the steady accumulation of broad sheets of lava, building up the shield volcano's distinctive form. Shield volcanoes are found wherever fluid low-silica lava reaches the surface of a rocky planet. However, they are most characteristic of ocean island volcanism associated with hot spots or with continental rift volcanism. They include the largest volcanoes on earth, such as Tamu Massif and Mauna Loa. Giant shield volcanoes are found on other planets of the Solar System, including Olympus Mons on Mars and Sapas Mons on Venus. Etymology The term 'shield volcano' is taken from the German term ''Schildvulkan'', coined by the Austrian geologist Eduard Suess in 1888 an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East African Rift
The East African Rift (EAR) or East African Rift System (EARS) is an active continental rift zone in East Africa. The EAR began developing around the onset of the Miocene, 22–25 million years ago. In the past it was considered to be part of a larger Great Rift Valley that extended north to Asia Minor. A narrow zone, the rift is a developing divergent tectonic plate boundary where the African Plate is in the process of splitting into two tectonic plates, called the Somali Plate and the Nubian Plate, at a rate of 6-7 mm per year. The rift system consists of three microplates, the Victoria Microplate to the north, and the Rovuma and Lwandle microplates to the south. The Victoria Microplate is rotating anti-clockwise with respect to the African plate. Its rotation is caused by the configuration of mechanically weaker and stronger lithospheric regions in the EARS. Extent A series of distinct rift basins, the East African Rift System extends over thousands of kilometers. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marsabit County
Marsabit County is a county in Kenya. Covering a surface area of 66,923.1 square kilometres. Marsabit is the second largest county in Kenya. Its capital is Marsabit and its largest town Moyale. According to the 2019 census, the county has a population of 459,785. It is bordered to the North by Ethiopia, to the West by Turkana County to the South by Samburu County and Isiolo County, and to the East by Wajir County. Geography The county is located in central north Kenya. It borders the eastern shore of Lake Turkana. Important topographical features are: Ol Donyo Ranges () in the southwest, Mount Marsabit () in the central part of the county, Hurri Hills () in the northeastern part of the county, Mount Kulal () in the northwest and the mountains around Sololo-Moyale escarpment (up to ) in the northeast. The Chalbi Desert makes up much of the center region of the county. Physical and tropical features The county is made of an extensive plain lying above sea level which gently sl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marsabit
Marsabit is a town in the northern Marsabit County in Kenya. It is situated in the former Eastern Province and is almost surrounded by the Marsabit National Park. The town is located east of the centre of the East African Rift at an elevation of between 1300 and 1400 metres. It serves as the capital of Marsabit County, and lies southeast of the Chalbi Desert in a forested area known for its volcanoes and crater lakes and others. Overview Marsabit is an outpost of urban civilization in the desert of northern Kenya. The town is situated on an isolated extinct volcano, Mount Marsabit, which rises almost a kilometer above the desert. The hills here are heavily forested, in contrast to the desert beyond, with their own "insular" eco-system. The town has a population of about 5,000. The town is mainly inhabited by the Cushitic-speaking Borana Oromo people. There are also very few Nilotic Turkana and Bantu Ameru residents. Additionally, there are also few non-Cushitic-speaking trade ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maar
A maar is a broad, low-relief volcanic crater caused by a phreatomagmatic eruption (an explosion which occurs when groundwater comes into contact with hot lava or magma). A maar characteristically fills with water to form a relatively shallow crater lake which may also be called a maar. The name comes from a Moselle Franconian dialect word used for the circular lakes of the Daun area of Germany. Notes: * According to German Wikipedia's ''"Maar"'' article, in 1544 in his book ''Cosmographia'', Sebastian Münster (1488–1552) first applied the word "maar" (as ''Marh'') to the Ulmener Maar and the Laacher See. See: Sebastian Münster, ''Cosmographia'' (Basel, Switzerland: Heinrich Petri, 1544)p. 341. From p. 341: ''"Item zwen namhafftiger seen seind in der Eyfel / einer bey de schloß Ulmen / und ein ander bey dem Closter züm Laich / die seind sere tieff / habe kein ynflüß aber vil außflüß / die nennet man Marh unnd seind fischreich."'' (Also two noteworthy lakes are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marsabit National Park
The Marsabit National Park is a national park and nature reserve located at Mount Marsabit in northern Kenya, near the town of Marsabit. It is located 560 km north of Nairobi in Marsabit County in the former Eastern Province and its reserve is noted for its zebra population and bird sanctuary. Geography The area contains a number of extinct volcanic craters, which are covered in forests. There is a crater in the vicinity named Gof Redo, roughly north of Marsabit in the fork of the roads to Moyale and North Horr. Flora and fauna Zebras, elephant, lions, giraffes, buffaloes, black and white colobus, blue monkeys, bushbucks, sunis, and leopards populate the park. The park contains some 350 species of birds in total, of which 52 are birds of prey. The cliffs in the northern end of Lake Paradise, in Gof Sokorte Gurda, are home to a number of birds, including Ruppell's griffon vultures, peregrine falcons, mountain buzzards, black kites and African fish eagles. Ducks such as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Martin And Osa Johnson
Martin Elmer Johnson (October 9, 1884 – January 13, 1937) and Osa Helen Johnson (née Leighty, March 14, 1894 – January 7, 1953) were married United States, American adventurers and documentary filmmakers. In the first half of the 20th century the couple captured the public's imagination through their films and books of adventure in exotic, faraway lands. Photographers, explorers, marketers, naturalists and authors, Martin and Osa studied the wildlife and peoples of East and Central Africa, the South Pacific Islands and British North Borneo. They explored then-unknown lands and brought back film footage and photographs, offering many Americans their first understanding of these distant lands. Early Lives Martin Elmer Johnson was born on October 9, 1884. Osa Leighty was born March 14, 1894, and raised in Chanute, Kansas. Although born in Rockford, Illinois, Martin Johnson grew up in the Kansas towns of Lincoln, Kansas, Lincoln and Independence, Kansas, Independence. His fathe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Volcanoes In Kenya ...
This is a short list of active and extinct volcanoes in Kenya.For a more comprehensive list of volcanoes and craters in Kenya, see :sw:Orodha ya volkeno nchini Kenya List of volcanoes in Kenya (non-exhaustive) References * Volcanoes of KenyVolcano Alive Retrieved on 2 November 2007 {{Kenya topics Kenya Volcanoes A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanoes Of Kenya
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
