Torres del Paine National Park is a national park encompassing a mountains, glacier, lake, and river-rich areas in southern Chilean Patagonia. The Cordillera del Paine is the centerpiece of the park. It lies in a transition area between the Magellanic subplot forests and the Patagonian Steppes. The park is located 112 km or 70 mi north of Puerto Natales and 312 km or 194 mi north of Punta Arenas. Bernardo O'Higgins National Park is its neighbour to the west, while Los Glaciares National Park is located to the north in Argentine territory.
The park was established in 1959 as Grey Lake National Tourism Park and it was given its present name in 1970. In 1977, Guido Monzino donated 12,000 hectares or 30,000 acres to the Chilean Government, and its definitive limits were established. The park was designated a World Biosphere Reserve by UNESCO in 1978. The landscape of the park is dominated by the Paine massif, which is an eastern spur of the Andes located on the east side of the Grey Glacier, rising dramatically above the Patagonian steppe. Small valleys separate the spectacular granite spires and mountains of the massif. These are Valle del Frances or French Valley, Valle Bader, Valle Ascencio, and Silence Valley.
The head of French Valley is a cirque formed by impressive cliffs. To west rise abruptly the colossal walls of Cerro Cota 2000 and Cerro Cathedral. Cerro Cota 2000 is named for its elevation; its highest contour line is about 2,000 m. Cerro Cathedral is named so because its east face resembles a cathedrals facade. Silence Valley is where standing face to face the gigantic granite walls of Cerro Fortaleza and Cerro Escudo with the western faces of the Torres del Paine. Ascencio Valley is the normal route to reach the Torres del Paine lookout, which is located at the bank of a milky green tarn. The highest mountain of the group is Paine Grande although its elevation has not been determined with precision.
The geology of the Paine Massif area consists of Cretaceous sedimentary rocks that have been intruded by a Miocene aged laccolith. Orogenic and erosional processes have shaped the present-day topography, glacial erosion being the main one responsible for the sculpturing of the massif in the last tens of thousands of years. A good example of the latter are the Cuernos del Paine, whose central bands of exposed granite strongly contrast with the dark aspect of their tops, which are remnants of a heavily eroded sedimentary stratum. In the case of Las Torres, what once was their overlying sedimentary rock layer has been completely eroded away, leaving behind the more resistant granite.
Torres del Paine National Park is adorned with beautiful vegetation. Among them are the evergreen Embothrium coccineum, which produces vivid red flowers grouped in corymbs and the Calceolaria uniflora, of striking shape and colors. The park has 7 documented species of Orchidaceae, including the Chloraea magellanica. In the park have been recorded 85 non-native plant species, of which 75 are of European origin and 31 are considered to be invasive. The park contains four vegetation zones Patagonian steppe, Pre-Andean shrubland, Magellanic deciduous forest and Andean Desert.
Guanacos are one of the most common mammals found in the park. Other mammals include cougars and foxes. It is also home to the endangered Chilean Huemul. The park contains breeding populations of 15 bird of prey species. Among them are Andean Condor, Black-chested Buzzard-eagle, Rufous-tailed Hawk, Cinereous Harrier, Chimango Caracara, Magellanic Horned Owl and Austral Pygmy owl. Other birds occurring in the park include the Chilean Flamingo, Darwin's Rhea, Coscoroba Swan, Black-necked Swan, Magellanic Woodpecker, Magellan Goose and Black-faced Ibis.
The national park is a popular hiking destination in Chile. There are clearly marked paths and many refugios which provide shelter and basic services. Views are breathtaking. Hikers can opt for a day trip to see the towers, walk the popular W route in about five days, or trek the full circle in 8–9 days. It is a national park and thus hikers are not allowed to stray from the paths. Camping is only allowed at specified campsites and wood fires are prohibited throughout the park.
Visiting the park is recommended between late December and late February, during the southern summer. Not only is the weather more hospitable, but daylight hours are very long given the extreme southern latitude. Outside of this time frame, the weather becomes too extreme for the majority of the public, and daylight dwindles to only a few hours a day. In 2005, a careless Czech back-packer used a gasoline stove in windy weather and caused a large fire that destroyed 160 km² of the park. Replanting, with assistance from the Czech Republic, was set to begin in September 2005. Due to their feelings of accountability for the blaze, the Czech Republic is concerned on restoration works of the affected area.
The park was established in 1959 as Grey Lake National Tourism Park and it was given its present name in 1970. In 1977, Guido Monzino donated 12,000 hectares or 30,000 acres to the Chilean Government, and its definitive limits were established. The park was designated a World Biosphere Reserve by UNESCO in 1978. The landscape of the park is dominated by the Paine massif, which is an eastern spur of the Andes located on the east side of the Grey Glacier, rising dramatically above the Patagonian steppe. Small valleys separate the spectacular granite spires and mountains of the massif. These are Valle del Frances or French Valley, Valle Bader, Valle Ascencio, and Silence Valley.The head of French Valley is a cirque formed by impressive cliffs. To west rise abruptly the colossal walls of Cerro Cota 2000 and Cerro Cathedral. Cerro Cota 2000 is named for its elevation; its highest contour line is about 2,000 m. Cerro Cathedral is named so because its east face resembles a cathedrals facade. Silence Valley is where standing face to face the gigantic granite walls of Cerro Fortaleza and Cerro Escudo with the western faces of the Torres del Paine. Ascencio Valley is the normal route to reach the Torres del Paine lookout, which is located at the bank of a milky green tarn. The highest mountain of the group is Paine Grande although its elevation has not been determined with precision.
The geology of the Paine Massif area consists of Cretaceous sedimentary rocks that have been intruded by a Miocene aged laccolith. Orogenic and erosional processes have shaped the present-day topography, glacial erosion being the main one responsible for the sculpturing of the massif in the last tens of thousands of years. A good example of the latter are the Cuernos del Paine, whose central bands of exposed granite strongly contrast with the dark aspect of their tops, which are remnants of a heavily eroded sedimentary stratum. In the case of Las Torres, what once was their overlying sedimentary rock layer has been completely eroded away, leaving behind the more resistant granite.
Torres del Paine National Park is adorned with beautiful vegetation. Among them are the evergreen Embothrium coccineum, which produces vivid red flowers grouped in corymbs and the Calceolaria uniflora, of striking shape and colors. The park has 7 documented species of Orchidaceae, including the Chloraea magellanica. In the park have been recorded 85 non-native plant species, of which 75 are of European origin and 31 are considered to be invasive. The park contains four vegetation zones Patagonian steppe, Pre-Andean shrubland, Magellanic deciduous forest and Andean Desert.
Guanacos are one of the most common mammals found in the park. Other mammals include cougars and foxes. It is also home to the endangered Chilean Huemul. The park contains breeding populations of 15 bird of prey species. Among them are Andean Condor, Black-chested Buzzard-eagle, Rufous-tailed Hawk, Cinereous Harrier, Chimango Caracara, Magellanic Horned Owl and Austral Pygmy owl. Other birds occurring in the park include the Chilean Flamingo, Darwin's Rhea, Coscoroba Swan, Black-necked Swan, Magellanic Woodpecker, Magellan Goose and Black-faced Ibis.The national park is a popular hiking destination in Chile. There are clearly marked paths and many refugios which provide shelter and basic services. Views are breathtaking. Hikers can opt for a day trip to see the towers, walk the popular W route in about five days, or trek the full circle in 8–9 days. It is a national park and thus hikers are not allowed to stray from the paths. Camping is only allowed at specified campsites and wood fires are prohibited throughout the park.
Visiting the park is recommended between late December and late February, during the southern summer. Not only is the weather more hospitable, but daylight hours are very long given the extreme southern latitude. Outside of this time frame, the weather becomes too extreme for the majority of the public, and daylight dwindles to only a few hours a day. In 2005, a careless Czech back-packer used a gasoline stove in windy weather and caused a large fire that destroyed 160 km² of the park. Replanting, with assistance from the Czech Republic, was set to begin in September 2005. Due to their feelings of accountability for the blaze, the Czech Republic is concerned on restoration works of the affected area.
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