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Santos Basin
The Santos Basin () is an approximately large mostly offshore sedimentary basin. It is located in the south Atlantic Ocean, some southeast of Santos, São Paulo, Santos, Brazil. The basin is one of the Brazilian basins to have resulted from the break-up of Gondwana since the Early Cretaceous, where a sequence of rift basins formed on both sides of the South Atlantic; the Pelotas, Santos, Campos and Espírito Santo Basins in Brazil, and the Namibia, Kwanza and Congo Basins in southwestern Africa. Santos Basin is separated from the Campos Basin to the north by the Cabo Frio High and the Pelotas Basin in the south by the Florianópolis High and the northwestern boundary onshore is formed by the Serra Do Mar coastal range. The basin is known for its thick layers of halite, salt that have formed structures in the subsurface due to halokinesis. The basin started forming in the Early Cretaceous on top of the Congo craton, Congo Craton as a rift basin. The rift stage of the basin evolu ...
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Santos, São Paulo
Santos (, ''Saints''), officially Municipality of Estância Balneária de Santos, is a city and Municipalities of Brazil, municipality in the Brazilian States of Brazil, state of São Paulo (state), São Paulo, founded in 1546 by the Portuguese nobleman Brás Cubas. It is located mostly on the São Vicente Island (São Paulo, Brazil), island of São Vicente, which harbors both the city of Santos and the city of São Vicente, São Paulo, São Vicente, and partially on the mainland. It is the main city in the metropolitan region of Baixada Santista. The population is 440,965 (2025 est.) in an area of . The city is home to the Coffee Museum, where world coffee prices were once negotiated. There is also a Soccer, football memorial, dedicated to the city's greatest players, which includes Pelé, who spent the majority of his career with Santos FC, Santos Futebol Clube. Its beachfront garden, in length, figures in ''Guinness World Records'' as the largest beachfront garden in the world. ...
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Atlantic Ocean
The Atlantic Ocean is the second largest of the world's five borders of the oceans, oceanic divisions, with an area of about . It covers approximately 17% of Earth#Surface, Earth's surface and about 24% of its water surface area. During the Age of Discovery, it was known for separating the New World of the Americas (North America and South America) from the Old World of Afro-Eurasia (Africa, Asia, and Europe). Through its separation of Afro-Eurasia from the Americas, the Atlantic Ocean has played a central role in the development of human society, globalization, and the histories of many nations. While the Norse colonization of North America, Norse were the first known humans to cross the Atlantic, it was the expedition of Christopher Columbus in 1492 that proved to be the most consequential. Columbus's expedition ushered in an Age of Discovery, age of exploration and colonization of the Americas by European powers, most notably Portuguese Empire, Portugal, Spanish Empire, Sp ...
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Panorama Aereo Itajai Balnerio Cambriu 2006 06
A panorama (formed from Greek πᾶν "all" + ὅραμα "view") is any wide-angle view or representation of a physical space, whether in painting, drawing, photography (panoramic photography), film, seismic images, or 3D modeling. The word was coined in the 18th century by the English ( Irish descent) painter Robert Barker to describe his panoramic paintings of Edinburgh and London. The motion-picture term ''panning'' is derived from ''panorama''. A panoramic view is also purposed for multimedia, cross-scale applications to an outline overview (from a distance) along and across repositories. This so-called "cognitive panorama" is a panoramic view over, and a combination of, cognitive spaces used to capture the larger scale. History The device of the panorama existed in painting, particularly in murals, as early as 20 A.D., in those found in Pompeii, as a means of generating an immersive " panoptic" experience of a vista. Cartographic experiments during the Enlighten ...
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Cabo Frio - Encanto
Cabo is Spanish, Portuguese and Galician for cape. It may refer to: * Cabo San Lucas, a resort city in Baja California Sur, Mexico * Cabó, a municipality in Alt Urgell, Lleida, Catalonia, Spain Other places * Cabo Blanco, Costa Rica * Cabo Corrientes (municipality), a municipality in Jalisco, Mexico * Cabo Delgado, a province of Mozambique * Cabo Frio, a Brazilian municipality * Cabo Orange National Park, Amapá, Brazil * Cabo Polonio, a hamlet in the Rocha Department, Uruguay * Cabo Rojo, Puerto Rico, a municipality situated on the southwest coast of Puerto Rico * Cabo Verde, the Portuguese name for Cape Verde * San José del Cabo, a city in Baja California Sur, Mexico, part of Los Cabos with Cabo San Lucas * Cabo de Goede Hoop, historic reference for Cape of Good Hope or The Cape in South Africa, with capital Cape Town Capes: * Cabo Branco Lighthouse, a cape in the extreme est of the entire Americas. Joao Pessoa, Brazil * Cabo Catoche, the northernmost point on the Yuc ...
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Jupiter Field
Jupiter is the fifth planet from the Sun and the List of Solar System objects by size, largest in the Solar System. It is a gas giant with a Jupiter mass, mass more than 2.5 times that of all the other planets in the Solar System combined and slightly less than one-thousandth the mass of the Sun. Its diameter is 11 times that of Earth and a tenth that of the Sun. Jupiter orbits the Sun at a distance of , with an orbital period of . It is the List of brightest natural objects in the sky, third-brightest natural object in the Earth's night sky, after the Moon and Venus, and has been observed since prehistoric times. Its name derives from that of Jupiter (god), Jupiter, the chief deity of ancient Roman religion. Jupiter was the first of the Sun's planets to form, and its inward migration during the primordial phase of the Solar System affected much of the formation history of the other planets. Jupiter's atmosphere consists of 76% hydrogen and 24% helium by mass, with a denser ...
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Libra Oil Field
Libra oil field is a large ultra-deepwater oil prospect located in the Santos Basin, about off the coast of Rio de Janeiro, Brazil, north of Tupi field. Libra is in the process of being tested and may turn out to be the largest pre-salt find in the basin, ahead of the Tupi oil field, making the largest find since Cantarell Field in 1976. National Agency of Petroleum (ANP) officials are confident Libra will contain even more recoverable oil than Franco oil field. History The field was discovered in May 2010 at the same time as the Franco prospect. Libra is located from Franco and is being drilled by Petrobras contracted by the ANP. Officials confirmed that Franco and Libra are not linked to the nearby Iara field. On 14 July 2010, the first exploration well collapsed when it reached an underwater salt bed. A second layer of hydrocarbons was found in late December 2010. Eleven companies including CNOOC, CNPC, Ecopetrol, Mitsui, ONGC Videsh (OVL), Petrogal, Petrobras, Pet ...
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Tupi Oil Field
The Tupi oil field (reverted from Lula oil field) is a large oil field located in the Santos Basin, off the coast of Rio de Janeiro, Brazil. The field was originally nicknamed in honor of the Tupi people and later named after the mollusc, however it was also ambiguously similar to the name of former Brazilian president Luiz Inácio Lula da Silva. It is considered to be the Western Hemisphere's largest oil discovery of the last 30 years. History left, Brazilian President Lula da Silva on the launch of the P-52 oil Platform The Tupi field was discovered in October 2006 by Petrobras. The former president of Brazil, Luiz Inácio Lula da Silva called the field ''second independence for Brazil''. The field was originally named Tupi but in 2010 it was renamed Lula. The name 'Lula' means squid in Portuguese but also refers to Luiz Inácio Lula da Silva. The upper estimate of of recoverable oil would be enough to meet the total global demand for crude oil for about three months ...
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Santos Basin
The Santos Basin () is an approximately large mostly offshore sedimentary basin. It is located in the south Atlantic Ocean, some southeast of Santos, São Paulo, Santos, Brazil. The basin is one of the Brazilian basins to have resulted from the break-up of Gondwana since the Early Cretaceous, where a sequence of rift basins formed on both sides of the South Atlantic; the Pelotas, Santos, Campos and Espírito Santo Basins in Brazil, and the Namibia, Kwanza and Congo Basins in southwestern Africa. Santos Basin is separated from the Campos Basin to the north by the Cabo Frio High and the Pelotas Basin in the south by the Florianópolis High and the northwestern boundary onshore is formed by the Serra Do Mar coastal range. The basin is known for its thick layers of halite, salt that have formed structures in the subsurface due to halokinesis. The basin started forming in the Early Cretaceous on top of the Congo craton, Congo Craton as a rift basin. The rift stage of the basin evolu ...
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Holocene
The Holocene () is the current geologic time scale, geological epoch, beginning approximately 11,700 years ago. It follows the Last Glacial Period, which concluded with the Holocene glacial retreat. The Holocene and the preceding Pleistocene together form the Quaternary period. The Holocene is an interglacial period within the ongoing Ice age, glacial cycles of the Quaternary, and is equivalent to Marine isotope stages, Marine Isotope Stage 1. The Holocene correlates with the last maximum axial tilt towards the Sun of the Earth#Axial tilt and seasons, Earth's obliquity. The Holocene corresponds with the rapid proliferation, growth, and impacts of the human species worldwide, including Recorded history, all of its written history, technological revolutions, development of major civilizations, and overall significant transition towards urban culture, urban living in the present. The human impact on modern-era Earth and its ecosystems may be considered of global significance for th ...
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Barremian
The Barremian is an age in the geologic timescale (or a chronostratigraphic stage) between 125.77 Ma (million years ago) and 121.4 ± 1.0 Ma (Historically, this stage was placed at 129.4 million to approximately 125 million years ago) It is a subdivision of the Early Cretaceous Epoch (or Lower Cretaceous Series). It is preceded by the Hauterivian and followed by the Aptian Stage.See Gradstein ''et al.'' (2004) or the online geowhen database (link below) Stratigraphic definitions The original type locality for the Barremian Stage is in the vicinity of the village of Barrême, Alpes-de-Haute-Provence, France. Henri Coquand defined the stage and named it in 1873. The base of the Barremian is determined by the first appearance of the ammonites '' Spitidiscus hugii'' and ''Spitidiscus vandeckii''. The end of the Barremian is determined by the geomagnetic reversal at the start of the M0r chronozone, which is biologically near the first appearance of the ammonite '' Paradesh ...
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Gondwana
Gondwana ( ; ) was a large landmass, sometimes referred to as a supercontinent. The remnants of Gondwana make up around two-thirds of today's continental area, including South America, Africa, Antarctica, Australia (continent), Australia, Zealandia, Arabian Peninsula, Arabia, and the Indian subcontinent. Gondwana was formed by the Accretion (geology), accretion of several cratons (large stable blocks of the Earth's crust), beginning   with the East African Orogeny, the collision of India and Geography of Madagascar, Madagascar with East Africa, and culminating in   with the overlapping Brasiliano orogeny, Brasiliano and Kuunga orogeny, Kuunga orogenies, the collision of South America with Africa, and the addition of Australia and Antarctica, respectively. Eventually, Gondwana became the largest piece of continental crust of the Paleozoic Era, covering an area of some , about one-fifth of the Earth's surface. It fused with Laurasia during the Carboniferous to form Pan ...
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South American Plate
The South American plate is a major tectonic plate which includes the continent of South America as well as a sizable region of the Atlantic Ocean seabed extending eastward to the African plate, with which it forms the southern part of the Mid-Atlantic Ridge. The easterly edge is a divergent boundary with the African plate; the southerly edge is a complex boundary with the Antarctic plate, the Scotia plate, and the Sandwich Plate; the westerly edge is a convergent boundary with the subducting Nazca plate; and the northerly edge is a boundary with the Caribbean plate and the oceanic crust of the North American plate. At the Chile triple junction, near the west coast of the Taitao– Tres Montes Peninsula, an oceanic ridge known as the Chile Rise is actively subducting under the South American plate. Geological research suggests that the South American plate is moving west away from the Mid-Atlantic Ridge: "Parts of the plate boundaries consisting of alternations of re ...
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