Portal:Bolivia
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IntroductionWelcome to the Bolivia portal
Bolivia, officially the Plurinational State of Bolivia, is a landlocked country located in central South America. It is a country with the largest geographic extension of Amazonian plains and lowlands, mountains and Chaco with a tropical climate, valleys with a warm climate, as well as being part of the Andes of South America and its high plateau areas with cold climates, hills and snow-capped mountains, with a wide biome in each city and region. It includes part of the Pantanal, the largest tropical wetland in the world, along its eastern border. It is bordered by Brazil to the north and east, Paraguay to the southeast, Argentina to the south, Chile to the southwest, and Peru to the west. The seat of government is La Paz, which contains the executive, legislative, and electoral branches of government, while the constitutional capital is Sucre, the seat of the judiciary. The largest city and principal industrial center is Santa Cruz de la Sierra, located on the Llanos Orientales (eastern tropical lowlands), a mostly flat region in the east of the country with a diverse non-Andean culture. The sovereign state of Bolivia is a constitutionally unitary state divided into nine departments. Its geography varies as the elevation fluctuates, from the western snow-capped peaks of the Andes to the eastern lowlands, situated within the Amazon basin. One-third of the country is within the Andean mountain range. With an area of 1,098,581 km2 (424,164 sq mi), Bolivia is the fifth-largest country in South America after Brazil, Argentina, Peru and Colombia, and, alongside Paraguay, is one of two landlocked countries in the Americas. It is the largest landlocked country in the Southern Hemisphere. The country's population, estimated at 12 million, is multiethnic, including Amerindians, Mestizos, and the descendants of Europeans and Africans. Spanish is the official and predominant language, although 36 indigenous languages also have official status, of which the most commonly spoken are Guaraní, Aymara, and Quechua. 20th century Bolivia experienced a succession of military and civilian governments until Hugo Banzer led a US-backed coup d'état in 1971, replacing the socialist government of Juan José Torres with a military dictatorship. Banzer's regime cracked down on left-wing and socialist opposition parties, and other perceived forms of dissent, resulting in the torturing and murders of countless Bolivian citizens. Banzer was ousted in 1978 and, twenty years later, returned as the democratically elected President of Bolivia (1997–2001). Under the 2006–2019 presidency of Evo Morales, the country saw significant economic growth and political stability but was also accused of democratic backsliding, and was described as a competitive authoritarian regime. Freedom House classifies Bolivia as a partly-free democracy as of 2023, with a 66/100 score. (Full article...) Selected article -Lake Tauca is a former lake in the Altiplano of Bolivia. It is also known as Lake Pocoyu for its constituent lakes: Lake Poopó, Salar de Coipasa and Salar de Uyuni. The lake covered large parts of the southern Altiplano between the Eastern Cordillera and the Western Cordillera, covering an estimated 48,000 to 80,000 square kilometres (19,000 to 31,000 sq mi) of the basins of present-day Lake Poopó and the Salars of Uyuni, Coipasa and adjacent basins. Water levels varied, possibly reaching 3,800 metres (12,500 ft) in altitude. The lake was saline. The lake received water from Lake Titicaca, but whether this contributed most of Tauca's water or only a small amount is controversial; the quantity was sufficient to influence the local climate and depress the underlying terrain with its weight. Diatoms, plants and animals developed in the lake, sometimes forming reef knolls. The duration of Lake Tauca's existence is uncertain. Research in 2011 indicated that the rise in lake levels began 18,500 BP, peaking 16,000 and 14,500 years ago. About 14,200 years ago, lake levels dropped before rising again until 11,500 years ago. Some researchers postulate that the last phase of Lake Tauca may have continued until 8,500 BP. The drying of the lake, which may have occurred because of the Bølling-Allerød climate oscillation, left the salt deposits of Salar de Uyuni. (Full article...) Did you know (auto-generated)
Selected pictureLake Titicaca
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