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Monte Fontainhas
Monte Fontainhas is a volcanic mountain in the middle of Brava island in Cape Verde. At 976 m elevation, it is the highest point of the island. Rock types are made up of phonolite and ignimbrite. The mountainous centre of the island is often covered with clouds, which feed numerous springs, as was already observed by the 19th century traveller Armand d'Avezac. See also *List of mountains in Cape Verde References Fontainhas Fontainhas is a settlement in the northern part of the island of Santo Antão, Cape Verde. It is situated near the rocky north coast of the island, 2 km southwest of Ponta do Sol and 19 km north of the island capital Porto Novo. The settlement in ... Geography of Brava, Cape Verde {{CapeVerde-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Instituto Nacional De Estatística (Cape Verde)
The Instituto Nacional de Estatística (Portuguese for the ''National Statistics Institute'', abbreviated as INE) is the public statistics institute of Cape Verde. Its current president is Osvaldo Rui Monteiro dos Reis Borges. The population censuses are held every first year of a decade; the most recent was in 2010. Its main office is on 18 Rua da Caixa Económica in the capital city of Praia. History Until 1975, under Portuguese rule, statistics were done by the Provincial Statistics Bureau (''Repartição Provincial de Estatística''), part of the Instituto Nacional de Estatística of Portugal. When Cape Verde became independent, the ''Serviço Nacional de Estatística'' (SNE, Portuguese for the National Statistics Service) was established, part of the Ministry of Economy. Its first president was Edgard Chrysostome Pinto. At the end of 1985, the Directorate-General of Statistics was created. In 1996, the new law of the National Statistics System was approved, and the ''Istituto ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains In Cape Verde ...
This is a list of mountains in Cabo Verde: List See also *Lists of mountains by region *Geography of Cape Verde Notes External links * {{Cape Verde topics * Cape Verde Mountains Cape A cape is a clothing accessory or a sleeveless outer garment which drapes the wearer's back, arms, and chest, and connects at the neck. History Capes were common in medieval Europe, especially when combined with a hood in the chaperon. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brava, Cape Verde
Brava (Portuguese for "wild" or "brave") is an island in Cape Verde, in the Sotavento group. At , it is the smallest inhabited island of the Cape Verde archipelago, but at the same time the greenest. First settled in the early 16th century, its population grew after Mount Fogo on neighbouring Fogo erupted in 1680. For more than a century, its main industry was whaling, but the island economy is now primarily agricultural. History Brava was discovered in 1462 by the Portuguese explorer Diogo Afonso.Valor simbólico do centro histórico da Praia Lourenço Conceição Gomes, Universidade Portucalense, 2008, p. 97 There is no evidence of human presence on the Cape Verde islands before the arrival of the Portuguese. Around 1620 the population of Brava started with the arrival of settlers from |
Stratovolcano
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain
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 (topography), 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 Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Verde
, national_anthem = () , official_languages = Portuguese , national_languages = Cape Verdean Creole , capital = Praia , coordinates = , largest_city = capital , demonym = Cape Verdean or Cabo Verdean , ethnic_groups_year = 2017 , government_type = Unitary semi-presidential republic , leader_title1 = President , leader_name1 = José Maria Neves , leader_title2 = Prime Minister , leader_name2 = Ulisses Correia e Silva , legislature = National Assembly , area_rank = 166th , area_km2 = 4033 , area_sq_mi = 1,557 , percent_water = negligible , population_census = 561,901 , population_census_rank = 172nd , population_census_year = 2021 , population_density_km2 = 123.7 , population_density_sq_mi = 325.0 , population_density_rank = 89th , GDP_PPP ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Phonolite
Phonolite is an uncommon extrusive rock, of intermediate chemical composition between felsic and mafic, with texture ranging from aphanitic (fine-grained) to porphyritic (mixed fine- and coarse-grained). Phonolite is a variation of the igneous rock trachyte that contains nepheline or leucite rather than quartz. Its intrusive equivalent is nepheline syenite. Phonolite is typically fine grained and compact. The name ''phonolite'' comes from the Ancient Greek meaning "sounding stone" due to the metallic sound it produces if an unfractured plate is hit; hence, the English name ''clinkstone'' is given as a synonym. Formation Unusually, phonolite forms from magma with a relatively low silica content, generated by low degrees of partial melting (less than 10%) of highly aluminous rocks of the lower crust such as tonalite, monzonite and metamorphic rocks. Melting of such rocks to a very low degree promotes the liberation of aluminium, potassium, sodium and calcium by melting of f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ignimbrite
Ignimbrite is a type of volcanic rock, consisting of hardened tuff. Ignimbrites form from the deposits of pyroclastic flows, which are a hot suspension of particles and gases flowing rapidly from a volcano, driven by being denser than the surrounding atmosphere. New Zealand geologist Patrick Marshall (1869-1950) coined the term ''ignimbrite'' from the Latin ''igni-'' [fire] and ''imbri-'' [rain]. Ignimbrites are made of a very poorly sorted mixture of volcanic ash (or tuff when Lithification, lithified) and pumice lapilli, commonly with scattered lithic fragments. The ash is composed of glass shards and crystal fragments. Ignimbrites may be loose and unconsolidated, or lithified (solidified) rock called lapilli-tuff. Near the volcanic source, ignimbrites often contain thick accumulations of lithic blocks, and distally, many show meter-thick accumulations of rounded cobbles of pumice. Ignimbrites may be white, grey, pink, beige, brown, or black depending on their composition and d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Armand D'Avezac
Armand refer to: People * Armand (name), list of people with this name * Armand (photographer) (1901–1963), Armenian photographer * Armand (singer) (1946–2015), Dutch protest singer *Sean Armand (born 1991), American basketball player * Armand, duc d'Aiguillon (1750–1800), French noble * Armand of Kersaint (1742–1793), French sailor and politician Places *Saint-Armand, Quebec, Canada * Armand-e Olya, Iran * Armand-e Sofla, Iran * Armand Rural District, Iran * St. Armand, New York *St. Armand's Key in Florida * Armand-Jude River, a river in Charlevoix Regional County Municipality, Capitale-Nationale, Quebec, Canada See also *Arman (other) *Arman (name) *Armand Commission, first commission of the European Atomic Energy Community *Armand de Brignac, champagne brand produced by Champagne Cattier *Armand's Legion, Continental Army military unit *St Armand (other) St-Armand, St. Armand, Saint Armand, or ''variation'', may refer to: People * Saint Herma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Firmin Didot
Firmin Didot (; 14 April 176424 April 1836) was a French printer, engraver, and type founder. Early life Firmin Didot was born in Paris into a family of printers founded by François Didot, the father of 11 children. Firmin was one of his grandchildren. The family's paper manufactory was located at Essonnes, a town c. 30 km southeast of Paris near Corbeil, which had notable paper factories. Work Didot invented the word "stereotype", which in printing refers to the metal printing plate created for the actual printing of pages (as opposed to printing pages directly with movable type), and used the process extensively, revolutionizing the book trade by his cheap editions. His manufactory was a place of pilgrimage for the printers of the world. He first used the process in his edition of Callet’s ''Tables of Logarithms'' (1795), in which he secured an accuracy till then unattainable. He published stereotyped editions of French, English and Italian classics at a very low p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Cape Verde
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 and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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