Photo Gallery

Fitz Roy (3375 m), one of the most beautiful Argentinean Andean peaks, rises in the Los Glaciares National Park (Santa Cruz province). Because of the harsh weather that prevails in the mountains, it is dangerous to climb. - 1973

Guanacos grazing on the pampas. The Fitz Roy massif in the background. - Santa Cruz Province - 1973

62 kilometres away from San Carlos de Bariloche, on the banks of the Limay River, lies Valle Encantado, a place with a special magic. Surrounded by mountains and rock formations that, letting the imagination run wild, come to life in the eyes of the beholder. - Neuquén Province - 1973

Argentina's soil holds real treasures, but has not yet been fully explored. Oil, however, has been extracted for years, in considerable quantities in the area of Comodoro Rivadavia province of Chubut on the southern coastal strip. If you follow the road from Buenos Aires to the southern tip, you will notice strange machines in the pampas, reminiscent of large grasshoppers, which are constantly pumping oil out of the earth's interior. Drilling rigs also rise up from the ocean. Comodoro Rivadavia is home to thousands of engineers, workers and employees who earn their living directly or indirectly from the oil deposits. The “black gold” is not refined in the city itself, but in La Plata, south of Buenos Aires. Comodoro Rivadavia's oil production covers part of the country's needs. Further drilling is being done in other provinces, especially in Mendoza and San Juan. - 1973

Mount Fitz Roy (3,375 m) was named in honour of the captain of the Beagle. It was under his command in 1834, following a sixteen-day boat journey on the Río Santa Cruz – in which Charles Darwin also took part – that this peak was first sighted. Towering some 1,600 metres above the surrounding plateau, it resembles a cluster of pillars and spires, whose vertical walls are separated by gorges a thousand metres deep. The Fitz Roy is rightly regarded as the most beautiful peak in the Andes. - Book: Picture 200 - Argentina - 1973

The western part of Patagonia is formed by the Andean Cordillera, which in certain sections presents an insurmountable barrier. The winds blow in from the Pacific in an almost constant direction. The clouds they carry gather over the high mountain peaks and bring heavy rainfall. This explains why, despite the relatively low altitude, glaciers – some of which are of immense proportions – stretch across the eastern flank of the Andes. In Los Glaciares National Park (Santa Cruz Province) lies Lago Argentino, the ‘Silver Lake’, one of the most beautiful lakes in this southern region. The town of Calafate on its southern shore is attracting ever more tourists. Several glaciers can be seen in the immediate vicinity. One is called Uppsala and is 40 kilometres long. Pictured here is the equally famous Perito Moreno. – Argentina – 1973

As the eastern tongue of the great Patagonian ice field, the 17-kilometre-long Moreno Glacier stretches down to the southern arm of Lago Argentino, where it ends in a 70-metre-high ice wall. Its scientific discoverer, R. Hauthal, had named it the ‘Bismarck Glacier’ in 1899; it was given its current name in honour of the Argentine naturalist F. P. Moreno. Even in Hauthal’s day, clear signs of irregular advances were evident, whilst the other Southern Andes glaciers were already retreating. Since then, the Canal de los Témpanos has been completely blocked on several occasions, leading to a build-up of water in the southern part of the lake and catastrophic flooding, prompting attempts – in vain – to blast the ice wall with bombs. It was only after a transverse crevasse had formed in the 2 to 2.5-kilometre-wide glacier tongue that the floodwaters drained away. Today, the ‘Canal de los Témpanos’ is open again. - Book: Picture 205 - Argentina - 1973

The western part of Patagonia is formed by the Andes Cordillera, which represents an insurmountable barrier in some sections. The winds blow from the Pacific in an almost unchanging direction. The clouds they bring accumulate above the high mountain peaks and cause abundant precipitation. This explains why, despite their low altitude, glaciers of sometimes enormous dimensions extend along the eastern flank of the Andes. In the Los Glaciares National Park (Santa Cruz Province) lies the Argentino, the Silver Lake, one of the most beautiful lakes in this southern region. The town of Calafate on its southern shore is visited by more and more tourists. Several glaciers can be seen nearby. One is called Uppsala and is 40 kilometres long. An equally famous one is called Perito Moreno. Navigation on the Silver Lake is dangerous, if only because of the wind and the storms that are frequent in the Cordillera. Nature, preserved in its authenticity, attracts many scientists who can devote themselves to their studies here. - 1973

As the eastern tongue of the great Patagonian ice field, the 17-kilometre-long Moreno Glacier stretches down to the southern arm of Lago Argentino, where it ends in a 70-metre-high ice wall. Its scientific discoverer, R. Hauthal, had named it the ‘Bismarck Glacier’ in 1899; it was given its current name in honour of the Argentine naturalist F. P. Moreno. Even in Hauthal’s day, clear signs of irregular advances were evident, whilst the other Southern Andes glaciers were already retreating. Since then, the Canal de los Témpanos has been completely blocked on several occasions, leading to a build-up of water in the southern part of the lake and catastrophic flooding, prompting attempts – in vain – to blast the ice wall with bombs. It was only after a transverse crevasse had formed in the 2 to 2.5-kilometre-wide glacier tongue that the floodwaters drained away. Today, the ‘Canal de los Témpanos’ is open again. - Book: Picture 204 - Argentina - 1973

The western part of Patagonia is formed by the Andes Cordillera, which represents an insurmountable barrier in some sections. The winds blow from the Pacific in an almost unchanging direction. The clouds they bring accumulate above the high mountain peaks and cause abundant precipitation. This explains why, despite their low altitude, glaciers of sometimes enormous dimensions extend along the eastern flank of the Andes. In the Los Glaciares National Park (Santa Cruz Province) lies the Argentino, the Silver Lake, one of the most beautiful lakes in this southern region. The town of Calafate on its southern shore is visited by more and more tourists. Several glaciers can be seen nearby. One is called Uppsala and is 40 kilometres long. An equally famous one is called Perito Moreno. Navigation on the Silver Lake is dangerous, if only because of the wind and the storms that are frequent in the Cordillera. Nature, preserved in its authenticity, attracts many scientists who can devote themselves to their studies here. - 1973

As the eastern tongue of the great Patagonian ice field, the 17-kilometre-long Moreno Glacier stretches down to the southern arm of Lago Argentino, where it ends in a 70-metre-high ice wall. Its scientific discoverer, R. Hauthal, had named it the ‘Bismarck Glacier’ in 1899; it was given its current name in honour of the Argentine naturalist F. P. Moreno. Even in Hauthal’s day, clear signs of irregular advances were evident, whilst the other Southern Andes glaciers were already retreating. Since then, the Canal de los Témpanos has been completely blocked on several occasions, leading to a build-up of water in the southern part of the lake and catastrophic flooding, prompting attempts – in vain – to blast the ice wall with bombs. It was only after a transverse crevasse had formed in the 2 to 2.5-kilometre-wide glacier tongue that the floodwaters drained away. Today, the ‘Canal de los Témpanos’ is open again. - Book: Picture 203 - Argentina - 1973

The Perito Moreno Glacier (Spanish: Glaciar Perito Moreno) is one of the best-known and most spectacular glaciers on Earth. It is situated in Los Glaciares National Park in the Argentine province of Santa Cruz, in south-western Patagonia. The glacier stretches for around 30 kilometres and is 5 kilometres wide. The impressive ice front rises, on average, 55 to 75 metres above the surface of Lago Argentino. Underwater, the ice extends a further 100 metres or so into the depths. Unlike most glaciers worldwide, which are shrinking due to global warming, the Perito Moreno Glacier is in a relatively stable equilibrium. It advances by up to 2 metres every day. As a result of this continuous movement, chunks of ice as tall as houses regularly break off from the front. This phenomenon is accompanied by a thunderous crash and a deep rumble that can be heard for kilometres. As it advances, the glacier periodically blocks a side arm of Lago Argentino (Brazo Rico). The dammed-up water builds up enormous pressure until the barrier finally collapses in a spectacular process lasting several days. – Argentina – 1973

As the eastern tongue of the great Patagonian ice field, the 17-kilometre-long Moreno Glacier stretches down to the southern arm of Lago Argentino, where it ends in a 70-metre-high ice wall. Its scientific discoverer, R. Hauthal, had named it the ‘Bismarck Glacier’ in 1899; it was given its current name in honour of the Argentine naturalist F. P. Moreno. Even in Hauthal’s day, clear signs of irregular advances were evident, whilst the other Southern Andes glaciers were already retreating. Since then, the Canal de los Témpanos has been completely blocked on several occasions, leading to a build-up of water in the southern part of the lake and catastrophic flooding, prompting attempts – in vain – to blast the ice wall with bombs. It was only after a transverse crevasse had formed in the 2 to 2.5-kilometre-wide glacier tongue that the floodwaters drained away. Today, the ‘Canal de los Témpanos’ is open again. - Book: Picture 202 - Argentina - 1973

Steam locomotive with coal trailer in Río Turbio - Province of Santa Cruz - 1973

The massive granodiorite batholith of the Southern Andes is dominated in the Chilean province of Magallanes by the Cordillera del Paine (2,460 m), which extends into Argentine territory. The towering rock spires, the Torres del Paine, consist of remnants of Cretaceous overlying strata that once covered the intrusive body that had risen from the depths. Contact metamorphism has greatly hardened the rock, making it particularly resistant to erosion. In the foreground is Laguna Amarga. The photograph was taken during the southern summer, on 10 January at 11 pm. - Book: Picture 5 - Argentina - 1975

The area surrounding the magnificent massifs, pinnacles and towers of the Cordillera del Paine has been a protected nature reserve for some time. The national park is one of the last refuges for guanacos still living in the wild. - Book: Picture 208 - Argentina - 1975

The area surrounding the magnificent massifs, pinnacles and towers of the Cordillera del Paine has been a protected nature reserve for some time. The small mountain lakes in Chile’s Torres del Paine National Park, such as Lago Nordenskjöld, owe their formation to the erosive action of Ice Age glaciers. - Book: Picture 207 - Argentina - 1975

A vast steppe with low vegetation (such as matahambre shrubs) tinged with autumnal red in the foreground, and the striking Cordillera del Paine mountain range with its snow-capped peaks in the background. We are in the Torres del Paine National Park in Chile. The turquoise lake is Lago Nordenskjöld, named after the Swedish geologist and polar explorer Otto Nordenskjöld, who conducted scientific research in the region at the end of the 19th century. – Chile – 1975

In southern Patagonia, and particularly in Tierra del Fuego and southern Chile, the climate and vegetation allow only sheep farming. The flocks graze scattered across thousands of hectares of stony wasteland. They are rounded up for just three occasions: disinfection baths, shearing and the slaughterhouse. But then the ovejeros, the shepherd gauchos, are often on the move for days on end with their powerful dogs, keeping in contact with one another via bonfires and smoke signals. – Torres del Paine National Park – Chile – 1975

Set against the backdrop of the Darwin Range in Chilean Tierra del Fuego, which rises to a height of 2,300 metres, a large valley glacier flows into the Admiralty Fjord. Two central moraines, formed by the confluence of tributary glaciers, appear as dark stripes. Icebergs drift from the pack ice field in front of the calving glacier tongue into the fjord, which flows into the Strait of Magellan. - Book: Picture 10 - Argentina - 1975