Portal:Geografía
 | Estado de mantenimiento del portal: (febrero de 2020)
|
El portal de geografía
La geografía (del griego antiguo γεωγραφία geōgraphía ; que combina gê «Tierra» y gráphō «escribir») es el estudio de las tierras, las características, los habitantes y los fenómenos de la Tierra . La geografía es una disciplina integral que busca comprender la Tierra y sus complejidades humanas y naturales , no solo dónde están los objetos, sino también cómo han cambiado y llegaron a ser. Si bien la geografía es específica de la Tierra, muchos conceptos se pueden aplicar de manera más amplia a otros cuerpos celestes en el campo de la ciencia planetaria . Se ha dicho que la geografía es "un puente entre las ciencias naturales y las disciplinas de las ciencias sociales ".
Los orígenes de muchos de los conceptos de la geografía se remontan al griego Eratóstenes de Cirene, quien pudo haber acuñado el término "geographia" ( c. 276 a. C. - c. 195/194 a. C. ). El primer uso registrado de la palabra γεωγραφία fue como título de un libro del erudito griego Claudio Ptolomeo (100 - 170 d. C.). Este trabajo creó la llamada "tradición ptolemaica" de la geografía, que incluía la "teoría cartográfica ptolemaica". Sin embargo, los conceptos de geografía (como la cartografía ) se remontan a los primeros intentos de comprender el mundo espacialmente, y el primer ejemplo de un intento de mapa del mundo data del siglo IX a. C. en la antigua Babilonia . La historia de la geografía como disciplina abarca culturas y milenios, siendo desarrollada independientemente por múltiples grupos y polinizada de forma cruzada por el comercio entre estos grupos. Los conceptos centrales de la geografía que son consistentes en todos los enfoques son el enfoque en el espacio, el lugar, el tiempo y la escala.
En la actualidad, la geografía es una disciplina extremadamente amplia con múltiples enfoques y modalidades. Ha habido múltiples intentos de organizar la disciplina, incluidas las cuatro tradiciones de la geografía, y en ramas. Las técnicas empleadas generalmente se pueden dividir en enfoques cuantitativos y cualitativos , y muchos estudios adoptan enfoques de métodos mixtos . Las técnicas comunes incluyen cartografía , teledetección , entrevistas y topografía . ( Artículo completo... )
Aquí se muestran artículos destacados , que representan algunos de los mejores contenidos de Wikipedia en inglés.
Imagen 1Caballería prusiana y austriaca luchando en la batalla de Mollwitz , por August Heinrich Ferdinand Tegetmeyer
La Primera Guerra de Silesia (en alemán: Erster Schlesischer Krieg ) fue una guerra entre Prusia y Austria que duró desde 1740 hasta 1742 y tuvo como resultado que Prusia se apoderara de la mayor parte de la región de Silesia (ahora en el suroeste de Polonia ) de manos de Austria. La guerra se libró principalmente en Silesia, Moravia y Bohemia (las tierras de la Corona de Bohemia ) y formó un teatro de la Guerra de Sucesión Austriaca más amplia . Fue la primera de las tres Guerras de Silesia libradas entre la Prusia de Federico el Grande y la Austria de María Teresa a mediados del siglo XVIII, las tres terminaron con el control prusiano de Silesia.
Ningún evento desencadenante en particular inició la guerra. Prusia citó sus reclamos dinásticos de siglos de antigüedad sobre partes de Silesia como casus belli , pero la Realpolitik y los factores geoestratégicos también jugaron un papel en la provocación del conflicto. La disputada sucesión de María Teresa a la monarquía de los Habsburgo brindó a Prusia la oportunidad de fortalecerse frente a sus rivales regionales, como Sajonia y Baviera . ( Artículo completo... )- Imagen 2
Macedonia ( / ˌ m æ s ɪ ˈ d oʊ n i ə / MASS-ih-DOH-nee-ə; Greek: Μακεδονία), also called Macedon (/ˈmæsɪdɒn/ MASS-ih-don), was an ancient kingdom on the periphery of Archaic and Classical Greece, which later became the dominant state of Hellenistic Greece. The kingdom was founded and initially ruled by the royal Argead dynasty, which was followed by the Antipatrid and Antigonid dynasties. Home to the ancient Macedonians, the earliest kingdom was centered on the northeastern part of the Greek peninsula, and bordered by Epirus to the southwest, Illyria to the northwest, Paeonia to the north, Thrace to the east and Thessaly to the south.
Before the 4th century BC, Macedonia was a small kingdom outside of the area dominated by the great city-states of Athens, Sparta and Thebes, and briefly subordinate to Achaemenid Persia. During the reign of the Argead king Philip II (359–336 BC), Macedonia subdued mainland Greece and the Thracian Odrysian kingdom through conquest and diplomacy. With a reformed army containing phalanxes wielding the sarissa pike, Philip II defeated the old powers of Athens and Thebes in the Battle of Chaeronea in 338 BC. Philip II's son Alexander the Great, leading a federation of Greek states, accomplished his father's objective of commanding the whole of Greece when he destroyed Thebes after the city revolted. During Alexander's subsequent campaign of conquest, he overthrew the Achaemenid Empire and conquered territory that stretched as far as the Indus River. For a brief period, his Macedonian Empire was the most powerful in the world – the definitive Hellenistic state, inaugurating the transition to a new period of Ancient Greek civilization. Greek arts and literature flourished in the new conquered lands and advances in philosophy, engineering, and science spread across the empire and beyond. Of particular importance were the contributions of Aristotle, tutor to Alexander, whose writings became a keystone of Western philosophy. (Full article...) - Image 3Calabozos is a Holocene caldera in central Chile's Maule Region (7th Region). Part of the Chilean Andes' volcanic segment, it is considered a member of the Southern Volcanic Zone (SVZ), one of the three distinct volcanic belts of South America. This most active section of the Andes runs along central Chile's western edge, and includes more than 70 of Chile's stratovolcanoes and volcanic fields. Calabozos lies in an extremely remote area of poorly glaciated mountains.
Calabozos and the majority of the Andean volcanoes formed from the subduction of the oceanic Nazca Plate under the continental South American continental lithosphere. The caldera is in a transitional region between thick and thin lithosphere, and is probably supplied by a pool of andesitic and rhyolitic magma. It sits on a historic bed of volcanic and plutonic sedimentary rock (rock formed within the Earth) that in turn sits on top of a layer of merged sedimentary and metamorphic rock. (Full article...) - Image 4
Manuel Marques de Sousa, Count of Porto Alegre (13 June 1804 – 18 July 1875), nicknamed "the Gloved Centaur", was an army officer, politician and abolitionist of the Empire of Brazil. Born into a wealthy family of military background, Manuel Marques de Sousa joined the Portuguese Army in Brazil in 1817 when he was little more than a child. His military initiation occurred in the conquest of the Banda Oriental (Eastern Bank), which was annexed and became the southernmost Brazilian province of Cisplatina in 1821. For most of the 1820s, he was embroiled in the Brazilian effort to keep Cisplatina as part of its territory: first during the struggle for Brazilian independence and then in the Cisplatine War. It would ultimately prove a futile attempt, as Cisplatina successfully separated from Brazil to become the independent nation of Uruguay in 1828.
A few years later, in 1835 his native province of Rio Grande do Sul was engulfed in a secessionist rebellion, the Ragamuffin War. The conflict lasted for almost ten years, and the Count was leading military engagements for most of that time. He played a decisive role in saving the provincial capital from the Ragamuffin rebels, allowing forces loyal to the legitimate government to secure a key foothold. In 1852, he led a Brazilian division during the Platine War in an invasion of the Argentine Confederation that overthrew its dictator. He was awarded a noble title, eventually raised from baron to viscount and finally to count. (Full article...) - Image 5The Mendip Hills as seen from Crook Peak near Compton Bishop
The Mendip Hills (commonly called the Mendips) is a range of limestone hills to the south of Bristol and Bath in Somerset, England. Running from Weston-super-Mare and the Bristol Channel in the west to the Frome valley in the east, the hills overlook the Somerset Levels to the south and the Chew Valley and other tributaries of the Avon to the north. The highest point, at 325 metres above sea level, is Beacon Batch which is the summit area atop Black Down. The hills gave their name to the former local government district of Mendip, which administered most of the local area until April 2023. The higher, western part of the hills, covering 198 km2 (76 sq mi) has been designated an Area of Outstanding Natural Beauty (AONB), which gives it a level of protection comparable to a national park.
The hills are largely formed from Carboniferous Limestone, which is quarried at several sites. Ash–maple woodland, calcareous grassland and mesotrophic grassland which can be found across the Mendip Hills provide nationally important semi-natural habitats. With their temperate climate these support a range of flora and fauna including birds, butterflies and small mammals. The dry stone walls that divide the pasture into fields are of botanical importance as they support important populations of the nationally scarce wall whitlowgrass (Draba muralis). (Full article...) - Image 6
Endurance under sail, Antarctic Ocean, c. 1915 Paget colour photograph by Frank Hurley
The Imperial Trans-Antarctic Expedition of 1914–1917 is considered to be the last major expedition of the Heroic Age of Antarctic Exploration. Conceived by Sir Ernest Shackleton, the expedition was an attempt to make the first land crossing of the Antarctic continent. After Roald Amundsen's South Pole expedition in 1911, this crossing remained, in Shackleton's words, the "one great main object of Antarctic journeyings". Shackleton's expedition failed to accomplish this objective but became recognized instead as an epic feat of endurance.
Shackleton had served in the Antarctic on the Discovery expedition of 1901–1904 and had led the Nimrod expedition of 1907–1909. In this new venture, he proposed to sail to the Weddell Sea and to land a shore party near Vahsel Bay, in preparation for a transcontinental march via the South Pole to the Ross Sea. A supporting group, the Ross Sea party, would meanwhile establish camp in McMurdo Sound and from there lay a series of supply depots across the Ross Ice Shelf to the foot of the Beardmore Glacier. These depots would be essential for the transcontinental party's survival, as the group would not be able to carry enough provisions for the entire crossing. The expedition required two ships: Endurance under Shackleton for the Weddell Sea party, and Aurora, under Aeneas Mackintosh, for the Ross Sea party. (Full article...) - Image 7
Jerome is a town in the Black Hills of Yavapai County in the U.S. state of Arizona. Founded in the late 19th century on Cleopatra Hill overlooking the Verde Valley, Jerome is more than 5,000 feet (1,500 m) above sea level. It is about 100 miles (160 km) north of Phoenix along State Route 89A between Sedona and Prescott. Supported in its heyday by rich copper mines, it was home to more than 10,000 people in the 1920s. As of the 2020 census, its population was 464.
The town owes its existence mainly to two ore bodies that formed about 1.75 billion years ago along a ring fault in the caldera of an undersea volcano. Tectonic plate movements, plate collisions, uplift, deposition, erosion, and other geologic processes eventually exposed the tip of one of the ore bodies and pushed the other close to the surface, both near Jerome. In the late 19th century, the United Verde Mine, developed by William A. Clark, extracted ore bearing copper, gold, silver, and other metals from the larger of the two. The United Verde Extension UVX Mine, owned by James Douglas Jr., depended on the other huge deposit. In total, the copper deposits discovered in Jerome's vicinity were among the richest ever found. (Full article...) - Image 8Portrait attributed to Simplício de Sá, c. 1830
Dom Pedro I (12 October 1798 – 24 September 1834) was the founder and first ruler of the Empire of Brazil, where he was known as "the Liberator". As King Dom Pedro IV, he reigned briefly over Portugal, where he also became known as "the Liberator" as well as "the Soldier King". Born in Lisbon, Pedro I was the fourth child of King Dom John VI of Portugal and Queen Carlota Joaquina, and thus a member of the House of Braganza. When the country was invaded by French troops in 1807, he and his family fled to Portugal's largest and wealthiest colony, Brazil.
The outbreak of the Liberal Revolution of 1820 in Lisbon compelled Pedro I's father to return to Portugal in April 1821, leaving him to rule Brazil as regent. He had to deal with challenges from revolutionaries and insubordination by Portuguese troops, all of which he subdued. The Portuguese government's threat to revoke the political autonomy that Brazil had enjoyed since 1808 was met with widespread discontent in Brazil. Pedro I chose the Brazilian side and declared Brazil's independence from Portugal on 7 September 1822. On 12 October, he was acclaimed Brazilian emperor and by March 1824 had defeated all armies loyal to Portugal. A few months later, Pedro I crushed the short-lived Confederation of the Equator, a failed secession attempt by provincial rebels in Brazil's northeast. (Full article...) - Image 9
Lock Haven is the county seat of Clinton County, in the U.S. state of Pennsylvania. Located near the confluence of the West Branch Susquehanna River and Bald Eagle Creek, it is the principal city of the Lock Haven Micropolitan Statistical Area, itself part of the Williamsport–Lock Haven combined statistical area. At the 2020 census, Lock Haven's population was 8,108.
Built on a site long favored by pre-Columbian peoples, Lock Haven began in 1833 as a timber town and a haven for loggers, boatmen, and other travelers on the river or the West Branch Canal. Resource extraction and efficient transportation financed much of the city's growth through the end of the 19th century. In the 20th century, a light-aircraft factory, a college, and a paper mill, along with many smaller enterprises, drove the economy. Frequent floods, especially in 1972, damaged local industry and led to a high rate of unemployment in the 1980s. (Full article...) - Image 10
The polar bear (Ursus maritimus) is a large bear native to the Arctic and nearby areas. It is closely related to the brown bear, and the two species can interbreed. The polar bear is the largest extant species of bear and land carnivore, with adult males weighing 300–800 kg (660–1,760 lb). The species is sexually dimorphic, as adult females are much smaller. The polar bear is white- or yellowish-furred with black skin and a thick layer of fat. It is more slender than the brown bear, with a narrower skull, longer neck and lower shoulder hump. Its teeth are sharper and more adapted to cutting meat. The paws are large and allow the bear to walk on ice and paddle in the water.
Polar bears are both terrestrial and pagophilic (ice-living) and are considered to be marine mammals because of their dependence on marine ecosystems. They prefer the annual sea ice but live on land when the ice melts in the summer. They are mostly carnivorous and specialized for preying on seals, particularly ringed seals. Such prey is typically taken by ambush; the bear may stalk its prey on the ice or in the water, but also will stay at a breathing hole or ice edge to wait for prey to swim by. The bear primarily feeds on the seal's energy-rich blubber. Other prey include walruses, beluga whales and some terrestrial animals. Polar bears are usually solitary but can be found in groups when on land. During the breeding season, male bears guard females and defend them from rivals. Mothers give birth to cubs in maternity dens during the winter. Young stay with their mother for up to two and a half years. (Full article...) - Image 11
Western Ganga was an important ruling dynasty of ancient Karnataka in India which lasted from about 350 to 1000 CE. They are known as "Western Gangas" to distinguish them from the Eastern Gangas who in later centuries ruled over Kalinga (modern Odisha and Northern Andhra Pradesh). The general belief is that the Western Gangas began their rule during a time when multiple native clans asserted their freedom due to the weakening of the Pallava empire in South India, a geo-political event sometimes attributed to the southern conquests of Samudra Gupta. The Western Ganga sovereignty lasted from about 350 to 550 CE, initially ruling from Kolar and later, moving their capital to Talakadu on the banks of the Kaveri River in modern Mysore district.
After the rise of the imperial Chalukyas of Badami, the Gangas accepted Chalukya overlordship and fought for the cause of their overlords against the Pallavas of Kanchi. The Chalukyas were replaced by the Rashtrakutas of Manyakheta in 753 CE as the dominant power in the Deccan. After a century of struggle for autonomy, the Western Gangas finally accepted Rashtrakuta overlordship and successfully fought alongside them against their foes, the Chola Dynasty of Tanjavur. In the late 10th century, north of Tungabhadra river, the Rashtrakutas were replaced by the emerging Western Chalukya Empire and the Chola Dynasty saw renewed power south of the Kaveri river. The defeat of the Western Gangas by Cholas around 1000 resulted in the end of the Ganga influence over the region. (Full article...) - Image 12
Johnson Creek is a 25-mile (40 km) tributary of the Willamette River in the Portland metropolitan area of the U.S. state of Oregon. Part of the drainage basin of the Columbia River, its catchment consists of 54 square miles (140 km2) of mostly urban land occupied by about 180,000 people as of 2012. Passing through the cities of Gresham, Portland, and Milwaukie, the creek flows generally west from the foothills of the Cascade Range through sediments deposited by glacial floods on a substrate of basalt. Though polluted, it is free-flowing along its main stem and provides habitat for salmon and other migrating fish.
Prior to European settlement, the watershed was heavily forested and was used by Native Americans of the Chinook band for fishing and hunting. In the 19th century, non-Native American settlers cleared much of the land for farming, and the stream is named for one of these newcomers, William Johnson, who in 1846 built a water-powered sawmill along the creek. By the early 20th century, a rail line parallel to the stream encouraged further residential and commercial development. As urban density increased in the floodplain, seasonal floods grew more damaging. In the 1930s the Works Progress Administration of the federal government lined the lower 15 miles (24 km) of Johnson Creek with rock to control the floods. Despite this, the creek flooded 37 times between 1941 and 2006. Since the 1990s, regional planners have tried to reduce flooding by controlling stormwater runoff, creating stream meanders, reducing erosion, replacing impervious surfaces, and protecting riparian buffers. (Full article...) - Image 13The Parthian Empire in 94 BC at its greatest extent, during the reign of Mithridates II (r. 124–91 BC)
The Parthian Empire (/ˈpɑːrθiən/), also known as the Arsacid Empire (/ˈɑːrsəsɪd/), was a major Iranian political and cultural power centered in ancient Iran from 247 BC to 224 AD. Its latter name comes from its founder, Arsaces I, who led the Parni tribe in conquering the region of Parthia in Iran's northeast, then a satrapy (province) under Andragoras, who was rebelling against the Seleucid Empire. Mithridates I (r. c. 171 – 132 BC) greatly expanded the empire by seizing Media and Mesopotamia from the Seleucids. At its height, the Parthian Empire stretched from the northern reaches of the Euphrates, in what is now central-eastern Turkey, to present-day Afghanistan and western Pakistan. The empire, located on the Silk Road trade route between the Roman Empire in the Mediterranean Basin and the Han dynasty of China, became a center of trade and commerce.
The Parthians largely adopted the art, architecture, religious beliefs, and regalia of their culturally heterogeneous empire, which encompassed Persian, Hellenistic, and regional cultures. For about the first half of its existence, the Arsacid court adopted elements of Greek culture, though it eventually saw a gradual revival of Iranian traditions. The Arsacid rulers were titled "King of Kings", claiming inheritance of the Achaemenid Empire; indeed, they accepted many local kings as vassals, although the Achaemenids would have had centrally appointed, albeit largely autonomous, satraps. The court did appoint a small number of satraps, largely outside Iran, but these satrapies were smaller and less powerful than the Achaemenid potentates. With the expansion of Arsacid power, the seat of central government shifted from Nisa to Ctesiphon along the Tigris (south of Baghdad), although several other sites also served as capitals. (Full article...) - Image 14A view of the MCVF, with Mount Cayley obscured by clouds on the left. Mount Fee is the relatively small jagged peak to the far right.
The Mount Cayley volcanic field (MCVF) is a remote volcanic zone on the South Coast of British Columbia, Canada, stretching 31 km (19 mi) from the Pemberton Icefield to the Squamish River. It forms a segment of the Garibaldi Volcanic Belt, the Canadian portion of the Cascade Volcanic Arc, which extends from Northern California to southwestern British Columbia. Most of the MCVF volcanoes were formed during periods of volcanism under sheets of glacial ice throughout the last glacial period. These subglacial eruptions formed steep, flat-topped volcanoes and subglacial lava domes, most of which have been entirely exposed by deglaciation. However, at least two volcanoes predate the last glacial period and both are highly eroded. The field gets its name from Mount Cayley, a volcanic peak located at the southern end of the Powder Mountain Icefield. This icefield covers much of the central portion of the volcanic field and is one of the several glacial fields in the Pacific Ranges of the Coast Mountains.
Eruptions along the length of the MCVF began between 1.6 and 5.3 million years ago. At least 23 eruptions have occurred throughout its eruptive history. This volcanic activity ranged from effusive to explosive, with magma compositions ranging from basaltic to rhyolitic. Because the MCVF has a high elevation and consists of a cluster of mostly high altitude, non-overlapping volcanoes, subglacial activity is likely to have occurred under less than 800 m (2,600 ft) of glacial ice. The style of this glaciation promoted meltwater escape during eruptions. The steep profile of the volcanic field and its subglacial landforms support this hypothesis. As a result, volcanic features in the MCVF that interacted with glacial ice lack rocks that display evidence of abundant water during eruption, such as hyaloclastite and pillow lava. (Full article...) - Image 15Image map of Kitchen Creek and its waterfalls in Ricketts Glen State Park, as well as other prominent features. Each label is linked to an article or image. Click here for larger map.
There are 24 named waterfalls in Ricketts Glen State Park in the U.S. state of Pennsylvania along Kitchen Creek as it flows in three steep, narrow valleys, or glens. They range in height from 9 feet (2.7 m) to the 94-foot (29 m) Ganoga Falls. Ricketts Glen State Park is named for R. Bruce Ricketts, a colonel in the American Civil War who owned over 80,000 acres (32,000 hectares) in the area in the late 19th and early 20th centuries, but spared the old-growth forests in the glens from clearcutting. The park, which opened in 1944, is administered by the Bureau of State Parks of the Pennsylvania Department of Conservation and Natural Resources (DCNR). Nearly all of the waterfalls are visible from the Falls Trail, which Ricketts had built from 1889 to 1893 and which the state park rebuilt in the 1940s and late 1990s. The Falls Trail has been called "the most magnificent hike in the state" and one of "the top hikes in the East". (Full article...)
.jpg/1280px-Civic_Building_(Jerome,_Arizona).jpg)
.jpg/1280px-Polar_Bear_-_Alaska_(cropped).jpg)
Artículos vitales para entender la Geografía.
.svg/1280px-South_America_(orthographic_projection).svg.png)
América del Sur es un continente que se encuentra en su totalidad en el hemisferio occidental y en su mayor parte en el hemisferio sur , con una porción considerablemente menor en el hemisferio norte . También se la puede describir como la subregión sur de las Américas . ( Artículo completo... )
Portales relacionados
Complicarse
Para obtener recursos para el editor y colaborar con otros editores para mejorar los artículos de Wikipedia relacionados con Geografía, visita WikiProject Geografía .
Imágenes seleccionadas
- Image 1Autor: John Mitchell ; escaneo: Biblioteca del Congreso, División de Geografía y Mapas.El mapa Mitchell es el mapa más completo del este de América del Norte realizado durante la era colonial . Mide aproximadamente 2,0 m de ancho por 1,4 m de alto y fue realizado por John Mitchell en 1757 en ocho hojas separadas. El mapa se utilizó durante el Tratado de París para definir los límites de los Estados Unidos y sigue siendo importante hoy en día para resolver disputas fronterizas.
- Image 2Map: Strebe, using GeocartThe Gall–Peters projection, named after James Gall and Arno Peters, is a specialization of a configurable equal-area map projection known as the cylindrical equal-area projection. It achieved considerable notoriety in the late 20th century as the centerpiece of a controversy surrounding the political implications of map design; Peters promoted it as a more faithful representation than the Mercator projection, which inflates the sizes of regions farther from the equator and thus makes the (mostly technologically underdeveloped) equatorial countries appear smaller and therefore, according to Peters, less significant.
- Image 3Credit: Martin WaldseemüllerThe Waldseemüller map is a map drawn by German cartographer Martin Waldseemüller originally published in April 1507. It was one of the first maps to chart latitude and longitude precisely, the first map to use the name "America", and the first to depict the Americas as separate from Asia.
- Image 4Map: Strebe, using GeocartThe equirectangular projection is a simple map projection attributed to Marinus of Tyre, who Ptolemy claims invented the projection about AD 100. The projection maps meridians to vertical straight lines of constant spacing, and circles of latitude to horizontal straight lines of constant spacing. The projection is neither equal area nor conformal. Because of the distortions introduced by this projection, it has few applications beyond base imagery to be reprojected to some more useful projection.
- Image 5Photo credit: Joaquim Alves GasparIllustration of the Ptolemaic geocentric model of the Universe (the theory that the Earth is the center of the universe) by Portuguese cosmographer and cartographer Bartolomeu Velho. Taken from his treatise Cosmographia, made in Paris, 1568. Notice the distances of the bodies to the centre of the Earth (left) and the times of revolution, in years (right).
- Image 6Map credit: Abraham CresquesThe Catalan Atlas is a medieval map in the Catalan language, created in 1375. Described as "the zenith of medieval map-work", it is the earliest known chart to use a compass rose. It was produced by the Majorcan cartographic school and is attributed to Abraham Cresques, a Jewish book illuminator described by a contemporary as a master of mappae mundi. It has been in the royal library of France (now the Bibliothèque nationale de France) since the time of King Charles V. The atlas originally consisted of six vellum leaves, each about 64.5 by 50 cm (25.4 by 19.7 in), folded vertically and painted in various colours including gold and silver. This picture is a montage of eight pages (four leaves) of the atlas, depicting Europe, northern Africa and Asia.
- Image 7Map: Strebe, using GeocartThe Hobo–Dyer projection is a cylindrical equal-area projection commissioned in 2002 by Bob Abramms and Howard Bronstein. This projection was drafted by cartographer Mick Dyer, who based it on the 1910 Behrmann projection.
- Image 8Map: Strebe, using GeocartThe Kavrayskiy VII projection is a map projection invented by Vladimir V. Kavrayskiy in 1939 as a general purpose pseudocylindrical projection. It produces maps with low overall distortion, despite its straight, evenly-spaced parallels and a simple formulation.
- Image 9Map: Diego Gutiérrez and Hieronymus CockAmericae Sive Quartae Orbis Partis Nova Et Exactissima Descriptio is an ornate geographical map of the Americas made in 1562 by Spanish cartographer Diego Gutiérrez and Flemish artist Hieronymus Cock. The map encompasses the eastern coast of North America, the whole of Central and South America, and parts of the western coasts of Europe and Africa. This is the earliest scale wall map of the New World and the first to use the name "California". Two extant copies are known.
- Image 10Map credit: Central Intelligence AgencyThe Robinson projection is a projection of a world map showing the entire Earth at once. It was specifically created in an attempt to find a good compromise to the problem of showing the whole globe as a single flat image. The projection was devised by Arthur H. Robinson in 1963; distortion is severe close to the poles, but quickly declines to moderate levels as latitudes decrease. This Robinson-projection map, with standard parallels of 38°N and 38°S, was produced by the United States Central Intelligence Agency and shows the world as of February 2016.
- Image 11Photo credit: NASAAntarctica, the continent surrounding the Earth's South Pole, is the coldest place on earth and is almost entirely covered by ice. Antarctica was discovered in late January 1820. Too cold and dry to support virtually any vascular plants, Antartica's flora presently consists of around 250 lichens, 100 mosses, 25-30 liverworts, and around 700 terrestrial and aquatic algal species.
- Image 12Map: Strebe, using GeocartThe azimuthal equidistant projection is an azimuthal map projection in which all points on the map are both proportionately correct distances from the center point and at the correct azimuth (direction) from the center point. Distances and directions to all places, however, are true only from the center point of projection. This projection has been used for the flag of the United Nations, for the USGS National Atlas of the United States of America, and for large-scale mapping of Micronesia, among others.
- Image 13A detailed eighteenth-century map of Scandinavia by J. B. Homann, depicting Denmark, Norway, Sweden, Finland and the Baltic states of Livonia, Latvia and Curlandia. The map notes fortified cities, villages, roads, bridges, forests, castles and topography. The elaborate title cartouche in the upper left quadrant features angels supporting a title curtain and a medallion supporting an alternative title in French, "Les Trois Covronnes du Nord".
Born in 1664, Homann became an engraver and cartographer in the late 17th century, and opened his own publishing house in 1702. In 1715 Emperor Charles VI appointed him Imperial Geographer of the Holy Roman Empire. Homann held the position until his death in 1724. - Image 14Map: Strebe, using GeocartThe Hammer retroazimuthal projection is a modified azimuthal proposed by Ernst Hermann Heinrich Hammer in 1910. As a retroazimuthal projection, azimuths (directions) are correct from any point to the designated center point. In whole-world presentation, the back and front hemispheres overlap, making the projection a surjective function. Here, the frontside and backside hemispheres, both with a 15° graticule and center point of 45°N, 90°W, are presented side-by-side.
- Image 15A composite relief satellite image of South America, the fourth-largest continent. South America occupies the southern portion of the landmass in the Western Hemisphere. The continent is generally delimited on the northwest by the Darién watershed along the Colombia–Panama border. Almost all of mainland South America sits on the South American Plate, as do nearby outlying islands.
Artículos biográficos destacados en geografía
Edward Wright ( bautizado el 8 de octubre de 1561; fallecido el 16 de noviembre de 1615) fue un matemático y cartógrafo inglésconocido por su libro Certaine Errors in Navigation (1599; 2.ª ed., 1610), que por primera vez explicó la base matemática de la proyección de Mercator basándose en los trabajos de Pedro Nunes , y estableció una tabla de referencia que proporcionaba el factor de multiplicación de la escala lineal en función de la latitud , calculado para cada minuto de arco hasta una latitud de 75°. Se trataba, de hecho, de una tabla de valores de la integral de la función secante , y era el paso esencial necesario para hacer práctico tanto la elaboración como el uso de las cartas de Mercator para la navegación.
Wright nació en Garveston , Norfolk , y estudió en el Gonville and Caius College de Cambridge , donde fue miembro de la facultad desde 1587 hasta 1596. En 1589, el colegio le concedió una licencia después de que Isabel I le pidiera que realizara estudios de navegación con una expedición de incursión organizada por el conde de Cumberland a las Azores para capturar galeones españoles . La ruta de la expedición fue el tema del primer mapa que se preparó según la proyección de Wright, que se publicó en Certaine Errors en 1599. Ese mismo año, Wright creó y publicó el primer mapa del mundo producido en Inglaterra y el primero en utilizar la proyección de Mercator desde el mapa original de Gerardus Mercator de 1569. ( Artículo completo... )
Sabías
¿Sabías esto sobre Geografía?
- ... que el libro de Johann Reinhold Forster de 1778, Observaciones realizadas durante un viaje alrededor del mundo, ha sido descrito como "el comienzo de la geografía moderna"?
- ...que la glaciación en Wisconsin hace 17 mil años ayudó a crear su geografía única ?
Lugares a tu alrededor
Los 10 artículos más populares del mes de WikiProject Geography
Los siguientes artículos relacionados con Geografía son los artículos más visitados de WikiProject Geografía . Consulte la lista completa en Wikipedia:WikiProject Geografía/Páginas populares .
- Image 1
Mapa de los Estados Unidos que muestra sus 50 estados , el distrito federal y cinco territorios habitados . Alaska, Hawái y los territorios se muestran en diferentes escalas, y las islas Aleutianas y las islas deshabitadas del noroeste de Hawái se omiten del mapa.
Los Estados Unidos de América son una república federal compuesta por 50 estados , un distrito federal ( Washington, DC , la capital de los Estados Unidos), cinco territorios principales y varias islas menores . Tanto los estados como los Estados Unidos en su conjunto son jurisdicciones soberanas. La Décima Enmienda de la Constitución de los Estados Unidos permite a los estados ejercer todos los poderes de gobierno no delegados al gobierno federal. Cada estado tiene su propia constitución y gobierno, y todos los estados y sus residentes están representados en el Congreso federal , una legislatura bicameral que consta del Senado y la Cámara de Representantes . Cada estado elige dos senadores, mientras que los representantes se distribuyen entre los estados en proporción al censo decenal más reciente ordenado por la constitución . Además, cada estado tiene derecho a seleccionar un número de electores para votar en el Colegio Electoral , el organismo que elige al presidente de los Estados Unidos , igual al total de representantes y senadores en el Congreso de ese estado. El Distrito Federal no tiene representantes en el Senado, pero tiene un delegado sin derecho a voto en la Cámara de Representantes y también tiene derecho a electores en el Colegio Electoral. El Congreso puede admitir más estados, pero no puede crear un nuevo estado a partir del territorio de un estado existente ni fusionar dos o más estados en uno solo sin el consentimiento de todos los estados involucrados, y cada nuevo estado es admitido en igualdad de condiciones con los estados existentes. ( Artículo completo... ) - Image 2Generation Z (often shortened to Gen Z), also known as Zoomers, is the demographic cohort succeeding Millennials and preceding Generation Alpha. Researchers and popular media use the mid-to-late 1990s as starting birth years and the early 2010s as ending birth years, with the generation most frequently being defined as people born from 1997 to 2012. Most members of Generation Z are the children of younger Baby Boomers or Generation X. (Full article...)
- Image 3The Blue Marble, Apollo 17, December 1972
Earth is the third planet from the Sun and the only astronomical object known to harbor life. This is enabled by Earth being an ocean world, the only one in the Solar System sustaining liquid surface water. Almost all of Earth's water is contained in its global ocean, covering 70.8% of Earth's crust. The remaining 29.2% of Earth's crust is land, most of which is located in the form of continental landmasses within Earth's land hemisphere. Most of Earth's land is somewhat humid and covered by vegetation, while large sheets of ice at Earth's polar deserts retain more water than Earth's groundwater, lakes, rivers and atmospheric water combined. Earth's crust consists of slowly moving tectonic plates, which interact to produce mountain ranges, volcanoes, and earthquakes. Earth has a liquid outer core that generates a magnetosphere capable of deflecting most of the destructive solar winds and cosmic radiation. (Full article...) - Image 4
Hong Kong is a special administrative region of the People's Republic of China. With 7.4 million residents of various nationalities in a 1,104-square-kilometre (426 sq mi) territory, Hong Kong is the fourth most densely populated region in the world. (Full article...) - Image 5
Dymaxion map of the world with the 30 largest countries and territories by area
This is a list of the world's countries and their dependencies by land, water, and total area, ranked by total area. (Full article...) - Image 6River Thames and Tower Bridge with The Shard and Southwark (left), and Tower of London and City of London (right)
London is the capital and largest city of both England and the United Kingdom, with a population of 8,866,180 in 2022. The wider metropolitan area is the largest in Western Europe, with a population of 14.9 million. London stands on the River Thames in southeast England, at the head of a 50-mile (80 km) estuary down to the North Sea, and has been a major settlement for nearly 2,000 years. Its ancient core and financial centre, the City of London, was founded by the Romans as Londinium and has retained its medieval boundaries. The City of Westminster, to the west of the City of London, has been the centuries-long host of the national government and parliament. London grew rapidly in the 19th century, becoming the world's largest city at the time. Since the 19th century, the name "London" has referred to the metropolis around the City of London, historically split between the counties of Middlesex, Essex, Surrey, Kent, and Hertfordshire, which since 1965 has largely comprised the administrative area of Greater London, governed by 33 local authorities and the Greater London Authority. (Full article...) - Image 7
Cartogram of the world's population in 2018; each square represents 500,000 people.
This is a list of countries and dependencies by population. It includes sovereign states, inhabited dependent territories and, in some cases, constituent countries of sovereign states, with inclusion within the list being primarily based on the ISO standard ISO 3166-1. For instance, the United Kingdom is considered a single entity, while the constituent countries of the Kingdom of the Netherlands are considered separately. In addition, this list includes certain states with limited recognition not found in ISO 3166-1. Also given in a percentage is each country's population compared with the world population, which the United Nations estimates at 8.119 billion as of 2024. (Full article...) - Image 8Generation X (often shortened to Gen X) is the demographic cohort following the Baby Boomers and preceding Millennials. Researchers and popular media often use the mid-1960s as its starting birth years and the late 1970s as its ending birth years, with the generation being generally defined as people born from 1965 to 1980. By this definition and U.S. Census data, there are 65.2 million Gen Xers in the United States as of 2019. Most of Generation X are the children of the Silent Generation and early Baby Boomers; Xers are also often the parents of Millennials and Generation Z. (Full article...)
- Image 9The United Nations uses three definitions for what constitutes a city, as not all cities in all jurisdictions are classified using the same criteria. Cities may be defined as the cities proper, the extent of their urban area, or their metropolitan regions. (Full article...)
- Image 10
Washington, D.C., formally the District of Columbia and commonly known as Washington or D.C., is the capital city and federal district of the United States. The city is on the Potomac River, across from Virginia, and shares land borders with Maryland to its north and east. It was named for George Washington, the first president of the United States. The district is named for Columbia, the female personification of the nation. (Full article...)
.jpeg/1280px-London_Skyline_(125508655).jpeg)
Imágenes destacadas
Artículos principales
Seleccione [►] para ver las subcategorías.
Wikimedia asociada
Los siguientes proyectos hermanos de la Fundación Wikimedia proporcionan más información sobre este tema:
Repositorio de medios libres Commons- Wikilibros
Libros de texto y manuales gratuitos - Wikidata
Base de conocimiento libre - Wikinoticias
Noticias de contenido libre
Colección de citas de Wikiquote
Biblioteca de contenido libre Wikisource- Wikiversidad
Herramientas de aprendizaje gratuitas - Wikivoyage
Guía de viaje gratuita
Diccionario y tesauro Wikcionario
Descubra Wikipedia a través de portales
.jpg){kind=link}
.jpg){kind=link}
.svg){kind=link}
.jpeg){kind=link}
