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Salão International Do Automóvel De São Paulo
Salão is a ''freguesia'' ("civil parish") in the municipality of Horta on the island of Faial, the Portuguese Azores. The population in 2011 was 401, in an area of 10.40 km². History The settlement of Salão can be traced back to 1620, to a Castilian family that moved there from the adjacent community of Santa Bárbara (now the area of ''Praça'' in Cedros). The family originally settled there in 1589, but after an acrimonious disagreement between neighbors, the family moved farther south. They constructed a new home in the zone that would be referred to as ''Carapeta''; ''Carapeta'' (or ''Carapeto'') is a disused term referring to ''"one who makes lies or liars"''. The nucleus of what would develop into Salão started in Carapeta, around the river-valleys that crossed the area. A local fountain ( pt, Fonte da Carapeta) supported the small community (of mostly Spanish settlers) in its infancy, until it was destroyed in the 1926 earthquake. They brought to the island ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Faial Island
Faial Island (), also known in English as Fayal, is a Portuguese island of the Central Group (Portuguese: ''Grupo Central'') of the Azores. The Capelinhos Volcano, the westernmost point of the island, may be considered the westernmost point of Europe, if the Monchique Islet, near Flores Island, is considered part of North America, for it sits on the North American Plate. Its largest town is Horta. With its nearest neighbours, Pico (east across the channel) and São Jorge (northeast across the channel), it forms an area commonly known as the ''Triângulo'' (English: ''Triangle''). The island has also been referred to as the Ilha Azul (English: ''Blue Island''), derived from the writings of Portuguese poet Raul Brandão, due to the large quantity of hydrangeas that bloom during the summer months: History During a period of medieval legends and unsubstantiated stories of mystical lands, the island of Faial first appeared on the 1375 Catalan Atlas, as Ilha da Ventura or ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nave
The nave () is the central part of a church, stretching from the (normally western) main entrance or rear wall, to the transepts, or in a church without transepts, to the chancel. When a church contains side aisles, as in a basilica-type building, the strict definition of the term "nave" is restricted to the central aisle. In a broader, more colloquial sense, the nave includes all areas available for the lay worshippers, including the side-aisles and transepts.Cram, Ralph Adams Nave The Catholic Encyclopedia. Vol. 10. New York: Robert Appleton Company, 1911. Accessed 13 July 2018 Either way, the nave is distinct from the area reserved for the choir and clergy. Description The nave extends from the entry—which may have a separate vestibule (the narthex)—to the chancel and may be flanked by lower side-aisles separated from the nave by an arcade. If the aisles are high and of a width comparable to the central nave, the structure is sometimes said to have three naves. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
São Jorge Island
São Jorge () is an island in the central group of the Azores archipelago and part of the autonomous region of Portugal. Separated from its nearest neighbours ( Pico and Faial islands) by the Pico-São Jorge Channel, the central group is often referred colloquially as part of the ''Triângulo'' ("Triangle") group or just "The Triangle". São Jorge is a relatively long thin island with tall cliffs, whose 8,381 inhabitants are concentrated on various geological debris fields (''fajãs'') along the north and south coasts; from east to west, the island is long and, north to south, wide: its area is . History It is unclear when the first explorers discovered the island of São Jorge; as part of the politics of human occupation, the Azores were populated after 1430 (probably 1439) through the initiative of Prince Henry the Navigator. 23 April, known as the feast day of Saint George, has been cited by historians as the reason for the island's name, although this is likely conj ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taro
Taro () (''Colocasia esculenta)'' is a root vegetable. It is the most widely cultivated species of several plants in the family Araceae that are used as vegetables for their corms, leaves, and petioles. Taro corms are a food staple in African, Oceanic, and South Asian cultures (similar to yams). Taro is believed to be one of the earliest cultivated plants. Names and etymology The English term '' taro'' was borrowed from the Māori language when Captain Cook first observed ''Colocasia'' plantations there in 1769. The form ''taro'' or ''talo'' is widespread among Polynesian languages:*''talo'': taro (''Colocasia esculenta'') – entry in the ''Polynesian Lexicon Project Online'' (Pollex). in Tahitian; ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lapilli
Lapilli is a size classification of tephra, which is material that falls out of the air during a volcanic eruption or during some meteorite impacts. ''Lapilli'' (singular: ''lapillus'') is Latin for "little stones". By definition lapilli range from in diameter. A pyroclastic particle greater than 64 mm in diameter is known as a volcanic bomb when molten, or a volcanic block when solid. Pyroclastic material with particles less than 2 mm in diameter is referred to as volcanic ash. Formation Lapilli are spheroid-, teardrop-, dumbbell- or button-shaped droplets of molten or semi-molten lava ejected from a volcanic eruption that fall to earth while still at least partially molten. These granules are not accretionary, but instead the direct result of liquid rock cooling as it travels through the air. Lapilli tuffs are a very common form of volcanic rock typical of rhyolite, andesite and dacite pyroclastic eruptions, where thick layers of lapilli can be deposited durin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyroclastic Flow
A pyroclastic flow (also known as a pyroclastic density current or a pyroclastic cloud) is a fast-moving current of hot gas and volcanic matter (collectively known as tephra) that flows along the ground away from a volcano at average speeds of but is capable of reaching speeds up to . The gases and tephra can reach temperatures of about . Pyroclastic flows are the most deadly of all volcanic hazards and are produced as a result of certain explosive eruptions; they normally touch the ground and hurtle downhill, or spread laterally under gravity. Their speed depends upon the density of the current, the volcanic output rate, and the gradient of the slope. Origin of term The word ''pyroclast'' is derived from the Greek (''pýr''), meaning "fire", and (''klastós''), meaning "broken in pieces". A name for pyroclastic flows which glow red in the dark is (French, "burning cloud"); this was notably used to describe the disastrous 1902 eruption of Mount Pelée on Martinique, a Fr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tephra
Tephra is fragmental material produced by a volcanic eruption regardless of composition, fragment size, or emplacement mechanism. Volcanologists also refer to airborne fragments as pyroclasts. Once clasts have fallen to the ground, they remain as tephra unless hot enough to fuse into pyroclastic rock or tuff. Tephrochronology is a geochronological technique that uses discrete layers of tephra—volcanic ash from a single eruption—to create a chronological framework in which paleoenvironmental or archaeological records can be placed. When a volcano explodes, it releases a variety of tephra including ash, cinders, and blocks. These layers settle on the land and, over time, sedimentation occurs incorporating these tephra layers into the geologic record. Often, when a volcano explodes, biological organisms are killed and their remains are buried within the tephra layer. These fossils are later dated by scientists to determine the age of the fossil and its place within the g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sand
Sand is a granular material composed of finely divided mineral particles. Sand has various compositions but is defined by its grain size. Sand grains are smaller than gravel and coarser than silt. Sand can also refer to a textural class of soil or soil type; i.e., a soil containing more than 85 percent sand-sized particles by mass. The composition of sand varies, depending on the local rock sources and conditions, but the most common constituent of sand in inland continental settings and non- tropical coastal settings is silica (silicon dioxide, or SiO2), usually in the form of quartz. Calcium carbonate is the second most common type of sand, for example, aragonite, which has mostly been created, over the past 500million years, by various forms of life, like coral and shellfish. For example, it is the primary form of sand apparent in areas where reefs have dominated the ecosystem for millions of years like the Caribbean. Somewhat more rarely, sand may be composed of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4). Clays develop plasticity when wet, due to a molecular film of water surrounding the clay particles, but become hard, brittle and non–plastic upon drying or firing. Most pure clay minerals are white or light-coloured, but natural clays show a variety of colours from impurities, such as a reddish or brownish colour from small amounts of iron oxide. Clay is the oldest known ceramic material. Prehistoric humans discovered the useful properties of clay and used it for making pottery. Some of the earliest pottery shards have been dated to around 14,000 BC, and clay tablets were the first known writing medium. Clay is used in many modern industrial processes, such as paper making, cement production, and chemical filtering. Between one-half and two-thirds of the world's population live or work in buildings made with clay, oft ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ribeirinha (Horta)
Ribeirinha is a ''freguesia'' ("civil parish") in the municipality of Horta in the Portuguese archipelago of the Azores. The population in 2011 was 427, in an area of 12.26 km2. It contains the localities Canadinha, Chã da Cruz, Espalhafatos, Lomba dos Espalhafatos and Rua da Igreja. History The parish receives its name from the small river and valley that was occupied during the period of settlement. Riberinha, in Portuguese, literally means small "ribeira", or small river-valley owing to its location. New settlers constructed their village two kilometers from the coast, due to several incursions by pirates. This distance allowed the inhabitants to monitor the coast and plan traps for the invaders. One area, ''Poceirão dos Mouros'', refers to one of these traps where the pirates (the ''Moors of the Canal'', as they were known) were ensnared. In 1643, as recounted by friar Diogo das Chagas, the parish consisted of 71 homes and 254 inhabitants. A quarter of a century la ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Horta, Azores
Horta () is a municipality and city in the Portuguese archipelago of the Azores encompassing the island of Faial. The population in 2011 was 15,038 in an area of The city of Horta itself has a population of about 7,000. Horta's marina is a primary stop for yachts crossing the Atlantic Ocean, and its walls and walkways are covered with paintings created by visitors noting the names of their vessels, crews, and the years they visited. Peter's Cafe Sport is a bar located across from the marina that houses the island's scrimshaw museum, a collection of artifacts carved from whale tooth and jawbone. Peter's is a point of reference for transatlantic yachters and sailors. History 15th through 17th centuries In 1467 the Flemish nobleman Josse van Huerter returned to Faial on a second expedition, this time disembarking along the shore of what would be known as Horta Bay. He built a small chapel which would later form the nucleus of a small community known as Horta, a name possibly d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iberian Union
pt, União Ibérica , conventional_long_name =Iberian Union , common_name = , year_start = 1580 , date_start = 25 August , life_span = 1580–1640 , event_start = War of the Portuguese Succession , event_end = Portuguese Restoration War , date_end = 1 December , year_end = 1640 , p1 = History of Portugal (1415–1578)Kingdom of Portugal , flag_p1 = Flag of Portugal (1578).svg , p2 = Crown of Castile , flag_p2 = Royal Banner of the Crown of Castile (Early Style)-Variant.svg , p3 = Crown of Aragon , flag_p3 = Royal Banner of Aragón.svg , p4 = Habsburg Spain , flag_p4 = Flag of Cross of Burgundy.svg , s1 = History of Portugal (1640–1777)Kingdom of Portugal , flag_s1 = Flag of Portugal (1640).svg , s2 = Habsburg Spain , flag_s2 = Flag of Cross of Burgundy.svg , image_coat = Full Ornamented Coat of Arms of Philip II of Spain (1580-1598).svg , image_map = Philip II's realms in 1598.png , ima ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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