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Geography of Chile

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Geography of Chile
Unknown author · CC BY-SA 3.0

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Through Geography, South America and Atlantic Ocean

Physical geography

The northern two-thirds of Chile lie on top of the telluric Nazca Plate, which, moving eastward about ten centimeters a year, is forcing its way under the continental plate of South America. This movement has resulted in the formation of the Peru–Chile Trench. At its deepest point, the trench descends to over 8,000 metres (26,000 ft).

The same telluric displacements that created the Peru-Chile Trench make the country prone to earthquakes. Between 1904 and 2020, Chile was struck by 478 earthquakes with a magnitude of 6+ on the Richter scale (13 of these had a magnitude of 8+). The strongest of these, known as the Great Chilean Earthquake, occurred in Valdivia in 1960 with a magnitude of 9.5. In 2010, the 27F Earthquake occurred with a magnitude of 8.8, causing extreme damage to south-central Chile. It caused a tsunami that destroyed several fishing villages in the south and raised or lowered sections of the coast as much as two meters. There are 12 other Chilean earthquakes on record with a magnitude of 8+.

The convergence between the Earth's surface plates has also generated the Andes, a geologically young mountain range that in Chilean territory alone includes about 620 volcanoes, many of which are active.

Approximately 80 percent of Chile's terrain consists of mountainous formations. Many of these mountains and volcanoes are part of the Andes range, while non-Andean mountains constitute parts of transverse and coastal ranges. The transverse ranges, notably found in the near north and far north natural regions, extend in diverse configurations from the Andes to the ocean, shaping valleys oriented in an east–west direction. The coastal ranges are predominantly visible in the central region of the country, contributing to the formation of the Central Valley (Valle Central) between these ranges and the Andes. In the southernmost reaches, the Central Valley merges with the waters of the ocean. Here, the elevated sections of the coastal range facing the Andes transform into a multitude of islands, creating a complex network of channels and fjords that have posed navigational challenges to seafarers.

Much of Chile's coastline is rugged. The Humboldt Current, which originates northwest of the Antarctic Peninsula (which juts into the Bellingshausen Sea) and runs the full length of the Chilean coast, makes the water cold. During the summer months, the temperature of the water off Chile's beaches in the central part of the country stays below 15 °C (59 °F). A recent global remote sensing analysis suggested that there were 564 km2 of tidal flats in Chile, making it the 44th-ranked country in the world in terms of tidal flat area.

Chilean territory extends as far west as Polynesia. The best known of Chile's Pacific islands is Easter Island (Isla de Pascua, also known by its Polynesian name of Rapa Nui), with a population of 2,800 people. Located 3,600 km (2,237 mi) west of Chile's mainland port of Caldera, just below the Tropic of Capricorn, Easter Island provides Chile with a gateway to the Pacific. It is noted for its 867 statues (moai), which are huge (up to twenty meters high) and sculpted from volcanic stone. These statues are believed to have played an important role in Rapa Nui’s religion and culture.

The Juan Fernández Islands, located 587 km (365 mi) west of Valparaíso, are the locale of a small fishing settlement.

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