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North Region (Cameroon)
The North Region () makes up 66,090 km2 of the northern half of The Republic of Cameroon. Neighbouring territories include the Far North Region to the north, the Adamawa Region to the south, Nigeria to the west, Chad to the east, and Central African Republic to the southeast. The city of Garoua is both the political and industrial capital. Garoua is Cameroon's third largest port, despite the fact that the Bénoué River upon which it relies is only navigable for short periods of the year. Major ethnic groups include the Fula or Fulani (; ), who are Islamic pastoralists, and numerous Muslim and animist speakers of Adamawa, Chadic, and Nilo-Saharan languages. French is the language of formal education, and Fulfulde, the language of the Fulbe, is widespread as a ''lingua franca''. Geography Land Bands of alternating metamorphic and sedimentary rock interspersed with granite characterise the north's geology. Granite covered in volcanic basalt makes up the southernmost r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Regions Of Cameroon
The Republic of Cameroon is divided into ten regions. History Between 1961 and 1972, Cameroon was a federal republic made up of two federated states, East Cameroon and West Cameroon. A unitary system came into being in 1972. The country was then divided into provinces. In 1983, Centre-South Province was divided into Centre and South and at the same time, Adamawa and Far North Provinces were split from North Province. See summary of administrative history in Zeitlyn 2018. In 2008, the President of the Republic of Cameroon, President Paul Biya signed decrees abolishing "provinces" and replacing them with "regions". Hence, all of the country's ten provinces are now known as regions. The Northwest region and Southwest region were granted special status in December 2019, giving them additional powers. File:Carte des États de la République fédérale du Cameroun.png, States of the Federal Republic of Cameroon (1961-1972) File:Cameroon provinces 1972-1983.png, Provinces ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ethnic Group
An ethnicity or ethnic group is a group of people with shared attributes, which they collectively believe to have, and long-term endogamy. Ethnicities share attributes like language, culture, common sets of ancestry, traditions, society, religion, history or social treatment. Ethnicities may also have a narrow or broad spectrum of genetic ancestry, with some groups having mixed genetic ancestry. ''Ethnicity'' is sometimes used interchangeably with ''nation'', particularly in cases of ethnic nationalism. It is also used interchangeably with '' race'' although not all ethnicities identify as racial groups. By way of assimilation, acculturation, amalgamation, language shift, intermarriage, adoption and religious conversion, individuals or groups may over time shift from one ethnic group to another. Ethnic groups may be divided into subgroups or tribes, which over time may become separate ethnic groups themselves due to endogamy or physical isolation from the parent gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adamawa Plateau
The Adamawa Plateau () is a plateau region in west-central Africa stretching from south-eastern Nigeria through north-central Cameroon ( Adamawa and North Provinces) to the Central African Republic. The part of the plateau that lies in Nigeria is more popularly known as Gotel Mountains. The Adamawa Plateau is the source of many waterways, including the Benue River. The average elevation is about , but elevations can reach as high as . It is important for its deposits of bauxite. The vegetation is mostly savanna. The endangered toad '' Amietophrynus djohongensis'' is known to exist in the wild only in the Cameroonian part of the Adamawa Plateau. The plateau is sparsely populated, and cattle raising is the main occupation in the area. The province and plateau were named after Fulani Muslim Muslims () are people who adhere to Islam, a Monotheism, monotheistic religion belonging to the Abrahamic religions, Abrahamic tradition. They consider the Quran, the foundational rel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial planet, rocky planet or natural satellite, moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of volcanism on Venus, Venus, which cover ~80% of the surface, are basaltic; the lunar mare, lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite ( ) is a coarse-grained (phanerite, phaneritic) intrusive rock, intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dike (geology), dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF diagram, QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) conta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock (geology), rock formed by the cementation (geology), cementation of sediments—i.e. particles made of minerals (geological detritus) or organic matter (biological detritus)—that have been accumulated or deposited at Earth's surface. Sedimentation is any process that causes these particles to settle in place. Geological detritus originates from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or Mass wasting, mass movement, which are called agents of denudation. Biological detritus is formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur when dissolved minerals precipitate from aqueous solution, water solution. The sedimentary rock cover of ... [...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 dist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lingua Franca
A lingua franca (; ; for plurals see ), also known as a bridge language, common language, trade language, auxiliary language, link language or language of wider communication (LWC), is a Natural language, language systematically used to make communication possible between groups of people who do not share a First language, native language or dialect, particularly when it is a third language that is distinct from both of the speakers' native languages. Linguae francae have developed around the world throughout human history, sometimes for commercial reasons (so-called "trade languages" facilitated trade), but also for cultural, religious, diplomatic and administrative convenience, and as a means of exchanging information between scientists and other scholars of different nationalities. The term is taken from the medieval Mediterranean Lingua Franca, a Romance languages, Romance-based pidgin language used especially by traders in the Mediterranean Basin from the 11th to the 19th c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fula Language
Fula ( ),Laurie Bauer, 2007, ''The Linguistics Student's Handbook'', Edinburgh also known as Fulani ( ) or Fulah (, , ; Adlam script, Adlam: , , ; Ajami script, Ajami: , , ), is a Senegambian languages, Senegambian language spoken by around 36.8 million people as a set of various dialects in a Dialect continuum, continuum that stretches across some 18 countries in West Africa, West and Central Africa. Along with other related languages such as Serer language, Serer and Wolof language, Wolof, it belongs to the Atlantic languages, Atlantic geographic group within Niger–Congo languages, Niger–Congo, and more specifically to the Senegambian languages, Senegambian branch. Unlike most Niger-Congo languages, Fula does not have Tone (linguistics), tones. It is spoken as a first language by the Fula people ("Fulani", ) from the Senegambia, Senegambia region and Guinea to Cameroon, Nigeria, and Sudan and by related groups such as the Toucouleur people in the Senegal River Valley ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nilo-Saharan Language
The Nilo-Saharan languages are a proposed family of around 210 African languages spoken by somewhere around 70 million speakers, mainly in the upper parts of the Chari and Nile rivers, including historic Nubia, north of where the two tributaries of the Nile meet. The languages extend through 17 nations in the northern half of Africa: from Algeria to Benin in the west; from Libya to the Democratic Republic of the Congo in the centre; and from Egypt to Tanzania in the east. As indicated by its hyphenated name, Nilo-Saharan is a family of the African interior, including the greater Nile Basin and the Central Sahara Desert. Eight of its proposed constituent divisions (excluding Kunama, Kuliak, and Songhay) are found in the modern countries of Sudan and South Sudan, through which the Nile River flows. In his book '' The Languages of Africa'' (1963), Joseph Greenberg named the group and argued it was a genetic family. It contained all the languages that were not included in the N ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chadic Language
The Chadic languages form a branch of the Afroasiatic language family. They are spoken in parts of the Sahel. They include 196 languages spoken across northern Nigeria, southern Niger, southern Chad, and northern Cameroon. By far the most widely spoken Chadic language is Hausa, a lingua franca of much of inland Eastern West Africa, particularly Niger and the northern half of Nigeria. Hausa is the only Chadic language with more than 1 million speakers. Composition Paul Newman (1977) classified the languages into the four groups which have been accepted in all subsequent literature. Further subbranching, however, has not been as robust; Roger Blench (2006), for example, only accepts the A/B bifurcation of East Chadic. Subsequent work by Joseph Lovestrand argues strongly that Kujarge is a valid member of East Chadic. The placing of Luri as a primary split of West Chadic is erroneous. Bernard Caron (2004) shows that this language is South Bauchi and part of the Polci cluster. A sugg ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adamawa Language
The Adamawa languages are a putative family of 80–90 languages scattered across the Adamawa Plateau in Central Africa, in northern Cameroon, north-western Central African Republic, southern Chad, and eastern Nigeria, spoken altogether by only one and a half million people (as of 1996). Joseph Greenberg classified them as one branch of the Adamawa–Ubangi family of Niger–Congo languages. They are among the least studied languages in Africa, and include many endangered languages; by far the largest is Mumuye, with 400,000 speakers. A couple of unclassified languages—notably Laal and Jalaa—are found along the fringes of the Adamawa area. Geographically, the Adamawa languages lie near the location of the postulated Niger–Congo – Central Sudanic contact that may have given rise to the Atlantic–Congo family, and so may represent the central radiation of that family. Classification Joseph Greenberg postulated the Adamawa languages as a part of Adamawa–Ubangian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
