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| Mountains of the Andes | |
|---|---|
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| Name | Andes |
| Country | Colombia, Venezuela, Ecuador, Peru, Bolivia, Chile, Argentina |
| Length km | 7000 |
| Highest | Aconcagua |
| Elevation m | 6961 |
Mountains of the Andes The Andes are the longest continental mountain range, running along the western edge of South America and influencing Andean civilizations, Spanish Empire, Inca Empire heritage and modern states such as Argentina and Chile. The chain shapes continental climate of Pacific Ocean margins, supports biodiversity hotspots like the Yungas and Puna grassland, and defines political borders including parts of Bolivia–Chile and Peru–Ecuador frontiers.
The Andes extend about 7,000 km from the vicinity of Lake Maracaibo in Venezuela through Colombia, Ecuador, Peru, and Bolivia to the southern tip of South America in Tierra del Fuego, influencing coastal features such as the Atacama Desert and inland basins like the Amazon Basin; major cities adjacent include Quito, Lima, La Paz, Cuzco, Santiago, and Mendoza. The cordillera divides into physiographic zones including the Cordillera Occidental (Colombia), Cordillera Central (Peru), and Cordillera Real with intermontane plateaus such as the Altiplano and basins like the Mantaro Valley, while islands of biodiversity include the Galápagos Islands influence via oceanic currents. Subranges such as the Cordillera Blanca, Cordillera Huayhuash, and Sierra Nevada del Cocuy create local climate gradients affecting river systems like the Marañón River and Bio-Bio River.
The Andes formed primarily through subduction of the Nazca Plate beneath the South American Plate with contributions from microplates such as the Caracas Basin and events like the Andean orogeny; major fault systems include the Santa Marta Fault and the Liquiñe-Ofqui Fault. Volcanism associated with the Ring of Fire produced stratovolcanoes like Ojos del Salado and Cotopaxi; uplift episodes during the Cenozoic and interactions with the Nazca Ridge and Juan Fernández Ridge influenced segmentation and crustal shortening documented in studies of the Sierras Pampeanas. Magmatic processes created mineralization linked to deposits exploited since pre-Columbian times and explored by entities such as CODELCO and Yanacocha.
Prominent peaks include Aconcagua (highest in the Americas), Huascarán, Ojos del Salado, Mount Pissis, Monte Pissis, and Nevado Sajama; ranges of note include the Cordillera Blanca, Cordillera Real, Andes of Colombia, Patagonian Andes, and the Northern Andes. Glaciated summits such as Alpamayo and Illimani are iconic for mountaineering histories involving expeditions like those led by Hans Kinzl and climbers documented in the archives of Alpine Club and national alpine federations; passes like the Paso de Jama and Abra de Porculla have shaped transportation routes connecting regions including Antofagasta and Jujuy.
Andean climates range from tropical montane climates near Quito and Medellín to polar tundra on high summits such as Nevado Huascarán; ecoregions include the Yungas, Montane grasslands and shrublands, Páramo, and Polylepis woodlands. Biodiversity hotspots host endemic taxa like species in the genera Andean condor (symbolic bird), Vicugna (camelids), and orchids described from the Sierra Nevada de Santa Marta region; ecological processes are shaped by altitudinal zonation, orographic precipitation influenced by the Humboldt Current, and cloud forest dynamics studied by institutions such as the Smithsonian Tropical Research Institute.
Human occupation spans prehistoric hunter-gatherers, the development of complex societies such as the Wari culture and the Tiwanaku, culminating in the Inca Empire which constructed road systems including the Qhapaq Ñan and sites like Machu Picchu. Spanish colonial administration reorganized land via viceroyalties like the Viceroyalty of Peru and introduced mining enterprises exemplified by Potosí and haciendas, shaping demographic and cultural syncretism manifested in festivals such as Inti Raymi and languages including Quechua and Aymara. Modern nation-states have contested Andean resources through corporations like Glencore and policy frameworks from bodies including the Organization of American States.
The Andes host world-class mineral deposits: copper centers like Chuquicamata and Escondida operated by firms including Codelco, gold-silver districts such as Yanacocha, and polymetallic mines around Potosí; hydrocarbon reserves occur in foothills of Venezuela and Colombia basins managed by companies like PDVSA and Ecopetrol. Agricultural terraces trace to pre-Columbian engineering at sites near Cusco and support crops such as potato varieties cataloged by the International Potato Center and quinoa commercialization linked to markets in La Paz and Lima; hydropower installations affect rivers exploited by utilities including EDELNOR and multinational investors.
Hazards include volcanic eruptions from systems like Cotopaxi and Nevado del Ruiz, seismic events associated with subduction megathrusts such as the 1960 Valdivia earthquake, landslides in zones like the Cordillera de Mérida, and glacial retreat documented on Quelccaya and Huascarán linked to climate change impacts assessed by agencies like the Intergovernmental Panel on Climate Change. Environmental challenges involve biodiversity loss in ecoregions such as Páramo, water security issues on the Altiplano, pollution from mining at sites including La Oroya, and socio-environmental conflicts engaging groups such as CONADE and indigenous organizations like the Aymara Nation.