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Fako
Mount Cameroon is an active volcano in the South West region of Cameroon next to the city of Buea near the Gulf of Guinea. Mount Cameroon is also known as Cameroon Mountain or Fako (the name of the higher of its two peaks) or by its indigenous name ''Mongo ma Ndemi'' ("Mountain of Greatness"). It is the highest point in sub-Saharan western and central Africa, the fourth-most prominent peak in Africa, and the 31st-most prominent in the world. The mountain is part of the area of volcanic activity known as the Cameroon Volcanic Line, which also includes Lake Nyos, the site of a disaster in 1986. The most recent eruption occurred on February 3, 2012. Description Mount Cameroon is one of Africa's largest volcanoes, rising to above the coast of west Cameroon. It rises from the coast through tropical rainforest to a bare summit, which is cold, windy, and occasionally dusted with snow. The massive steep-sided volcano of dominantly basaltic-to-trachybasaltic composition forms a volc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southwest Region (Cameroon)
The Southwest Region or South-West Region () is a region in Cameroon. Its capital is Buea. , its population was 1,553,320. Along with the Northwest Region, it is one of the two Anglophone (English-speaking) regions of Cameroon. Various Ambazonian nationalist and separatist factions regard the ''Sud-Ouest'' region as being distinct as a polity from Cameroon. Administration The region is divided into six divisions or departments: Fako, Koupé-Manengouba, Lebialem, Manyu, Meme, and Ndian. These are in turn broken down into subdivisions. Presidentially appointed senior divisional officers () and subdivisional officers () govern each respectively. Ambazonian separatism Separatists from the Ambazonia administration regard both the Nord-Ouest (Northwest) and Sud-Ouest (Southwest) regions as being constituent components of their envisaged breakaway state. Geography The region was notable for having the first English-speaking university in Cameroon (the University of Buea). Towns i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Buea
Buea is the capital of the Southwest Region of Cameroon. The city is located in Fako Division, on the eastern slopes of Mount Cameroon, and has a population of 300,000 (at the 2013 Census). It has two Government Hotels, the Mountain Hotel and Parliamentarian Flats Hotel located around The Government Residential Area. The self-declared state of Ambazonia claims the city as its capital. History Buea, originally "bue", was founded by a hunter who came from the Bomboko area. Coming from the Bomboko side of the mountain, he named the new-found land in amazement as "a Bue", meaning literally a "son of bué". A prominent King of the tikar clashes with German troops during invasion. Resistance remain popular folklore; currently ruled by the Endeleys. Tea growing is an important local industry, especially in Tole. Buea was the colonial capital of German Kamerun from 1901 to 1919, the capital of the Southern Cameroons from 1949 until 1961 and the capital of West Cameroon until 1972, whe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ambazonian
Ambazonia, officially the Federal Republic of Ambazonia, also referred to as Amba Land, is an unrecognised breakaway state in West Africa which claims the Northwest Region and Southwest Region of Cameroon, though it currently controls almost none of the claimed territory. No country has formally recognized Ambazonia's independence, and it is currently the site of an armed conflict between Ambazonian separatist guerrillas and the Cameroonian military known as the Anglophone Crisis. Ambazonia is located in the west of Cameroon and southeast of Nigeria on the Gulf of Guinea. Until 1961, the region was a British colony, Southern Cameroons, while the rest of Cameroon was a French colony, French Cameroon. At independence, a plebiscite was held, and voters in Southern Cameroons opted to join Cameroon as a constituent state of a federal republic. Over time, the power of the central government, dominated by Francophones, expanded at the expense of the region's autonomy. Many inhabita ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
SRTM
The Shuttle Radar Topography Mission (SRTM) is an international research effort that obtained digital elevation models on a near-global scale from 56°S to 60°N, to generate the most complete high-resolution digital topographic database of Earth prior to the release of the ASTER GDEM in 2009. SRTM consisted of a specially modified radar system that flew on board the Space Shuttle Endeavour during the 11-day STS-99 mission in February 2000. The radar system was based on the older '' Spaceborne Imaging Radar-C/X-band Synthetic Aperture Radar'' (SIR-C/X-SAR), previously used on the Shuttle in 1994. To acquire topographic data, the SRTM payload was outfitted with two radar antennas. One antenna was located in the Shuttle's payload bay, the other – a critical change from the SIR-C/X-SAR, allowing single-pass interferometry – on the end of a 60-meter (200-foot) mast that extended from the payload bay once the Shuttle was in space. The technique employed is known as interferomet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precambrian
The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the Phanerozoic Eon, which is named after Cambria, the Latinised name for Wales, where rocks from this age were first studied. The Precambrian accounts for 88% of the Earth's geologic time. The Precambrian is an informal unit of geologic time, subdivided into three eons ( Hadean, Archean, Proterozoic) of the geologic time scale. It spans from the formation of Earth about 4.6 billion years ago ( Ga) to the beginning of the Cambrian Period, about million years ago ( Ma), when hard-shelled creatures first appeared in abundance. Overview Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian fossil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metamorphic Rock
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock. Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's land surface. They are classified by their protolith, their chemical and mineral makeup, and their texture. They may be formed simply by being deeply buried beneath the Earth's surface, where they are subject to high temperatures and the great pressure of the rock layers above. They can also form from tectonic processes such as continental collisions, which cause horizontal pressure, friction, and distorti ... [...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] |
Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today, although a third epoch, the Anthropocene, has been proposed but is not yet officially recognised by the ICS). The Quaternary Period is typically defined by the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. Research history In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive formations or "orders" ( it, quattro ordini). The term "quaternary" was introduced by Jules Desnoye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carthage
Carthage was the capital city of Ancient Carthage, on the eastern side of the Lake of Tunis in what is now Tunisia. Carthage was one of the most important trading hubs of the Ancient Mediterranean and one of the most affluent cities of the classical world. The city developed from a Canaanite Phoenician colony into the capital of a Punic empire which dominated large parts of the Southwest Mediterranean during the first millennium BC. The legendary Queen Alyssa or Dido, originally from Tyre, is regarded as the founder of the city, though her historicity has been questioned. According to accounts by Timaeus of Tauromenium, she purchased from a local tribe the amount of land that could be covered by an oxhide. As Carthage prospered at home, the polity sent colonists abroad as well as magistrates to rule the colonies. The ancient city was destroyed in the nearly-three year siege of Carthage by the Roman Republic during the Third Punic War in 146 BC and then re-developed as Roman Car ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Mount Cameroon
Little Mount Cameroon, also known as Etinde, is a peak on the southern flank of Mount Cameroon Mount Cameroon is an active volcano in the South West region of Cameroon next to the city of Buea near the Gulf of Guinea. Mount Cameroon is also known as Cameroon Mountain or Fako (the name of the higher of its two peaks) or by its indigenous n .... References Mount Cameroon Mountains of Cameroon Volcanoes of Cameroon Southwest Region (Cameroon) {{Africa-mountain-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Africa
Africa is the world's second-largest and second-most populous continent, after Asia in both cases. At about 30.3 million km2 (11.7 million square miles) including adjacent islands, it covers 6% of Earth's total surface area and 20% of its land area.Sayre, April Pulley (1999), ''Africa'', Twenty-First Century Books. . With billion people as of , it accounts for about of the world's human population. Africa's population is the youngest amongst all the continents; the median age in 2012 was 19.7, when the worldwide median age was 30.4. Despite a wide range of natural resources, Africa is the least wealthy continent per capita and second-least wealthy by total wealth, behind Oceania. Scholars have attributed this to different factors including geography, climate, tribalism, colonialism, the Cold War, neocolonialism, lack of democracy, and corruption. Despite this low concentration of wealth, recent economic expansion and the large and young population make Afr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hanno The Navigator
Hanno the Navigator (sometimes "Hannon"; xpu, 𐤇𐤍𐤀 , ; ) was a Carthaginian explorer of the fifth century BC, best known for his naval exploration of the western coast of Africa. The only source of his voyage is a ''periplus'' translated into Greek. He has sometimes been identified as a king. Historians have attempted to identify places on Hanno's route based on the ''periplus''. According to some modern analyses of his route, Hanno's expedition could have reached as far south as Gabon; however, according to others, it could not have taken him further than southern Morocco. Biography The name Hanno was given to many other Carthaginians. Ancient authors who discussed Hanno the Navigator did not provide direct information to identify him exactly. Some called him king, and others used the Latin words ''dux'' (leader or general) or '' imperator'' (commander or emperor).. The Greek translation of Hanno's ''periplus'' account names him a '' basileus'',. a term which may ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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