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Cova (crater)
Cova is a volcanic caldera in the eastcentral part of the island of Santo Antão in Cape Verde. It is situated at the southwestern end of the municipality of Paul. Its lowest point is 1,166 meters, and the highest point of the crater rim is about 1,500 m. The diameter of the caldera is about 1.0 km. It forms a part of Cova-Paul-Ribeira da Torre Natural Park.Parques Naturais Áreas protegidas Cabo Verde The Cova formation dates from between 1.4 million and 700,000 years ago. The Cova crater benefits from high precipitation values carried by trade winds. At the bottom of the caldera maize and beans are grown. Natural and semi-natural vegetation occupies the crater walls facing north and northeast. South facing walls are covered with a forest of '' |
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] |
Santo Antão, Cape Verde
Santo Antão (Portuguese for " Saint Anthony") is the westernmost island of Cape Verde. At , it is the largest of the Barlavento Islands group, and the second largest island of Cape Verde.Cabo Verde, Statistical Yearbook 2015 Instituto Nacional de Estatística The nearest island is São Vicente to the southeast, separated by the sea channel Canal de São Vicente. Its population was 38,200 in mid 2019, [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Caldera
A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is gone. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface (from one to dozens of kilometers in diameter). Although sometimes described as a Volcanic crater, crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur each century, the formation of a caldera is a rare event, occurring only a few times per century. Only seven caldera-forming collapses are known to have occurred between 1911 and 2016. More recently, a caldera collapse occurred at Kīlauea, Hawaii in 2018. Etymology The term ''caldera'' comes from Spanish language, S ... [...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] |
Paul, Cape Verde
Paul is a ''concelho'' (municipality) of Cape Verde. Situated in the northeastern part of the island of Santo Antão, it covers 7% of the island area (54.3 km2), and is home to 16% of its population (6,997 at the 2010 census). Its seat is the town Pombas. The municipality and parish The municipality consists of one ''freguesia'' (civil parish), Santo António das Pombas. The ''freguesia'' is subdivided into the following settlements (population at the 2010 census): * Cabo da Ribeira (pop: 912) * Campo de Cão (pop: 787) *Eito (pop: 979) *Figueiral (pop: 591) * Janela (pop: 1,658) *Pico da Cruz (pop: 138) * Pombas (pop: 1,295, city)Cabo Verde, Statistical Yearbook 2015 [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cova-Paul-Ribeira Da Torre Natural Park
Cova-Paul-Ribeira da Torre Natural Park, in the east of the island of Santo Antão, is one of ten "natural parks" in the country of Cape Verde.Parques Naturais Áreas protegidas Cabo Verde Its area is ,Resolução nº 36/2016 Estratégia e Plano Nacional de Negócios das Áreas Protegidas of which in the municipality of Ribeira Grande, in the municipality of and in the municipali ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pinus
A pine is any conifer tree or shrub in the genus ''Pinus'' () of the family Pinaceae. ''Pinus'' is the sole genus in the subfamily Pinoideae. The World Flora Online created by the Royal Botanic Gardens, Kew and Missouri Botanical Garden accepts 187 species names of pines as current, together with more synonyms. The American Conifer Society (ACS) and the Royal Horticultural Society accept 121 species. Pines are commonly found in the Northern Hemisphere. ''Pine'' may also refer to the lumber derived from pine trees; it is one of the more extensively used types of lumber. The pine family is the largest conifer family and there are currently 818 named cultivars (or trinomials) recognized by the ACS. Description Pine trees are evergreen, coniferous resinous trees (or, rarely, shrubs) growing tall, with the majority of species reaching tall. The smallest are Siberian dwarf pine and Potosi pinyon, and the tallest is an tall ponderosa pine located in southern Oregon's Rogue Riv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cupressus
''Cupressus'' is one of several genera of evergreen conifers within the family Cupressaceae that have the common name cypress; for the others, see cypress. It is considered a polyphyletic group. Based on genetic and morphological analysis, the genus ''Cupressus'' is found in the subfamily Cupressoideae. The common name "cypress" comes via the Old French ''cipres'' from the Latin ''cyparissus'', which is the latinisation of the Greek κυπάρισσος (''kypárissos''). Taxonomy There has long been significant uncertainty about the New World members of ''Cupressus'', with several studies recovering them as forming a distinct clade from the Old World members. A 2021 molecular study found ''Cupressus'' to be the sister genus to ''Juniperus'', whereas the western members (classified in '' Callitropsis'' and ''Hesperocyparis'') were found to be sister to ''Xanthocyparis''. Description They are evergreen trees or large shrubs, growing to 5–40 m tall. The leaves are scale-lik ... [...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] |
Cabo Da Ribeira
Cabo da Ribeira is a settlement in the eastern part of the island of Santo Antão, Cape Verde. In 2010 its population was 912. It is situated at about 500 m elevation in the upper valley of the Ribeira do Paul, 5 km southwest of Pombas. It is part of the municipality of Paul, and lies in the Cova-Paul-Ribeira da Torre Natural Park. See also *List of villages and settlements in Cape Verde This is a list of villages and smaller settlements in Cape Verde: Boa Vista * Bofarreira * Cabeça dos Tarrafes * Curral Velho - abandoned settlement * Espingueira - abandoned settlement * Estância de Baixo * Fundo das Figueiras * João ... References Villages and settlements in Santo Antão, Cape Verde Paul, Cape Verde Cova-Paul-Ribeira da Torre Natural Park {{CapeVerde-geo-stub ... [...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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