Perito Moreno Glacier, one of the most important tourist attractions in the Argentine Patagonia

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el_calafate_map Perito Moreno Glacier ( [show location on an interactive map] 50°29′S, 73°03′W) is a glacier located in the Los Glaciares National Park in the south west of Santa Cruz province, Argentina. It is one of the most important tourist attractions in the Argentine Patagonia.

The 250 km² ice formation, of 30 km in length, is one of 48 glaciers fed by the Southern Patagonian Ice Field located in the Andes system shared with Chile. This icefield is the world's third largest reserve of fresh water.
Satellite image of the Glacier. Note the colour difference between both sides of the lake.


Satellite image of the Glacier. Note the colour difference between both sides of the lake.

The Perito Moreno Glacier is one of only three Patagonian glaciers that are not retreating. Periodically the glacier advances over the L-shaped "Lago Argentino" ("Argentine Lake") forming a natural dam which separates the two halves of the lake when it reaches the opposite shore.

With no escape route, the water-level on the Brazo Rico side of the lake can rise by up to 30 meters above the level of the main lake. The enormous pressure produced by this mass of waters finally breaks the ice barrier holding it back, in a spectacular rupture event. This dam/rupture cycle is not regular and it naturally recurs at any frequency between once a year to less than once a decade.


The glacier on the shore 2 weeks before the 2004 rupture.

The terminus of the Perito Moreno Glacier is 5 km wide, with an average height of 60 meters above the surface of the water, with a total ice depth of 170 meters. It advances at a speed of up to 2 m per day (around 700 m per year), although it loses mass at approximately the same rate, meaning that aside from small variations, its terminus has not advanced or receded in the past 90 years. At its deepest part, the glacier has a depth of approximately 700 m.

The glacier first ruptured in 1917, taking with it an ancient forest of arrayán (Luma apiculata) trees. The last rupture occurred in March 2006, and previously in 2004, 1988, 1984, 1980, 1977, 1975, 1972, 1970, 1966, 1963, 1960, 1956, 1953, 1952, 1947, 1940, 1934 and 1917. It ruptures, on average, about every four to five years.

The Perito Moreno glacier, located 78 km from El Calafate, was named after the explorer Francisco Moreno, a pioneer who studied the region in the 19th century and played a major role in defending the territory of Argentina in the conflict surrounding the international border dispute with Chile.

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The Aiguille du Midiis a mountain in the Mont Blanc massif in the French Alps

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The Aiguille du Midi (3,842 m) is a mountain in the Mont Blanc massif in the French Alps.

The cable car to the summit, the Téléphérique de l'Aiguille du Midi, was built in 1955 and held the title of the world's highest cable car for about two decades. It still holds the record as the highest vertical ascent cable car in the world, from 1035m to 3842m. It travels from Chamonix to the top of the Aiguille du Midi – an altitude gain of over 2,800 m – in 20 minutes.

The Aiguille summit contains a panoramic viewing platform, a cafe and a gift shop. The Vallée Blanche ski run begins here, and the nearby Cosmiques Refuge is the starting point for one of the routes to the Mont Blanc summit. From the Aiguille another cable car (summer months only) crosses the Glacier de Geant to Point Helbronner (3,452 m) at the Italian side of the Mont Blanc Massif. Point Helbronner is served with a cable car from La Palud, a village near Courmayeur in the Aosta Valley (Italy).

The name "Aiguille du Midi" translates literally as "needle of midday". It is so called as the sun sits directly over the peak at noon, when viewed from Chamonix.


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Yosemite National Park, renowned for its magnificent valley, great granite domes and peaks, waterfalls, giant sequoias, and spectacular high country

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Yosemite National Park is a national park spanning eastern portions of Tuolumne, Mariposa and Madera counties in east central California, United States. The park covers an area of 761,266 acres or 1,189 square miles (3,081 km²) and reaches across the western slopes of the Sierra Nevada mountain chain.Yosemite is visited by over 3.5 million people each year, many of whom only spend time in the seven square miles (18 km²) of Yosemite Valley.

Designated a World Heritage Site in 1984, Yosemite is internationally recognized for its spectacular granite cliffs, waterfalls, clear streams, Giant Sequoia groves, and biological diversity] Almost 95% of the park is designated wilderness. Although not the first designated national park, Yosemite was a focal point in the development of the national park idea, largely owing to the work of people like John Muir and Galen Clark.

The geology of the Yosemite area is characterized by granitic rocks and remnants of older rock. About 10 million years ago, the Sierra Nevada was uplifted and then tilted to form its relatively gentle western slopes and the more dramatic eastern slopes. The uplift increased the steepness of stream and river beds, resulting in formation of deep, narrow canyons. About 1 million years ago, snow and ice accumulated, forming glaciers at the higher alpine meadows that moved down the river valleys. Ice thickness in Yosemite Valley may have reached 4,000 feet (1200 m) during the early glacial episode. The downslope movement of the ice masses cut and sculpted the U-shaped valley that attracts so many visitors to its scenic vistas today.

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