Portal:Chile

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The Chile Portal

The flag of Chile

Chile, officially the Republic of Chile, is a country in western South America. It is the southernmost country in the world and the closest to Antarctica, stretching along a narrow strip of land between the Andes Mountains and the Pacific Ocean. With an area of 756,102 square kilometers (291,933 sq mi) and a population of 17.5 million as of 2017, Chile shares borders with Peru to the north, Bolivia to the northeast, Argentina to the east, and the Drake Passage to the south. The country also controls several Pacific islands, including Juan Fernández, Isla Salas y Gómez, Desventuradas, and Easter Island, and claims about 1,250,000 square kilometers (480,000 sq mi) of Antarctica as the Chilean Antarctic Territory. The capital and largest city of Chile is Santiago, and the national language is Spanish.

Spain conquered and colonized the region in the mid-16th century, replacing Inca rule, but failed to conquer the independent Mapuche people who inhabited what is now south-central Chile. Chile emerged as a relatively stable authoritarian republic in the 1830s after their 1818 declaration of independence from Spain. During the 19th century, Chile experienced significant economic and territorial growth, putting an end to Mapuche resistance in the 1880s and gaining its current northern territory in the War of the Pacific (1879–83) by defeating Peru and Bolivia. In the 20th century, up until the 1970s, Chile underwent a process of democratization and experienced rapid population growth and urbanization, while relying increasingly on exports from copper mining to support its economy. During the 1960s and 1970s, the country was marked by severe left-right political polarization and turmoil, which culminated in the 1973 Chilean coup d'état that overthrew Salvador Allende's democratically elected left-wing government. This was followed by a 16-year right-wing military dictatorship under Augusto Pinochet, which resulted in more than 3,000 deaths or disappearances. The regime ended in 1990, following a referendum in 1988, and was succeeded by a center-left coalition, which ruled until 2010.

Chile has a high-income economy and is one of the most economically and socially stable nations in South America, leading Latin America in competitiveness, per capita income, globalization, peace, and economic freedom. Chile also performs well in the region in terms of sustainability of the state and democratic development, and boasts the second lowest homicide rate in the Americas, following only Canada. Chile is a founding member of the United Nations, the Community of Latin American and Caribbean States (CELAC), and the Pacific Alliance, and joined the OECD in 2010. (Full article...)

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Socompa as seen from near the Salar de Imilac.

Socompa is a large stratovolcano at the border of Argentina and Chile with an elevation of 6,051 metres (19,852 ft) metres. Part of the Chilean and Argentine Andean Volcanic Belt (AVB), it is within the Central Volcanic Zone, one of the various segments of the AVB. This part of the Andean volcanic belt begins in Peru and runs first through Bolivia and Chile, and then through Argentina and Chile, and contains about 44 active volcanoes. Socompa lies close to the pass of the same name, where the Salta-Antofagasta railway crosses the border.

Socompa is known for its large debris avalanche, which was formed 7,200 years ago when most of the northwestern slope collapsed and slid down, forming an extensive deposit. It was at first considered to be either a moraine or a nuee ardende deposit, until the 1980 eruption of Mount St. Helens prompted awareness of the instability of volcanic edifices and the existence of large scale collapses on them. The Socompa collapse is among the largest known with a volume of 19.2 cubic kilometres (4.6 cu mi) and covers a surface area of 490 square kilometres (190 sq mi), and its features are well preserved by the arid climate. Notable are the large toreva blocks which were left behind within the collapse crater. After the landslide, the volcano was rebuilt by the effusion of lava flows and much of the scar is now filled in. (Full article...)

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Neruda in 1963

Pablo Neruda (/nəˈruːdə/ nə-ROO-də; Spanish pronunciation: [ˈpaβlo neˈɾuða] ⓘ; born Ricardo Eliécer Neftalí Reyes Basoalto; 12 July 1904 – 23 September 1973) was a Chilean poet-diplomat and politician who won the 1971 Nobel Prize in Literature. Neruda became known as a poet when he was 13 years old and wrote in a variety of styles, including surrealist poems, historical epics, political manifestos, a prose autobiography, and passionate love poems such as the ones in his collection Twenty Love Poems and a Song of Despair (1924).

Neruda occupied many diplomatic positions in various countries during his lifetime and served a term as a senator for the Chilean Communist Party. When President Gabriel González Videla outlawed communism in Chile in 1948, a warrant was issued for Neruda's arrest. Friends hid him for months in the basement of a house in the port city of Valparaíso, and in 1949, he escaped through a mountain pass near Maihue Lake into Argentina; he would not return to Chile for more than three years. He was a close advisor to Chile's socialist president Salvador Allende, and when he got back to Chile after accepting his Nobel Prize in Stockholm, Allende invited him to read at the Estadio Nacional before 70,000 people. (Full article...)

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Nevados de Putre, Taapaca volcano (right)

Taapaca is a Holocene volcanic complex in northern Chile's Arica y Parinacota Region. Located in the Chilean Andes, it is part of the Central Volcanic Zone of the Andean Volcanic Belt, one of four distinct volcanic chains in South America. The town of Putre lies at the southwestern foot of the volcano.

Like other volcanoes of the Central Volcanic Zone, Taapaca formed from the subduction of the Nazca Plate beneath the South America Plate. It lies on the western margin of the Altiplano high plateau, on top of older volcanic and sedimentary units. Taapaca has mainly erupted dacite, in the form of numerous lava domes, although an andesitic stratovolcano is also present. (Full article...)
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