Photo Gallery

The Chilean Puna de Atacama, situated between San Pedro de Atacama and the Tatio geysers, is a monotonous high plateau formed from rhyolitic lava. The bitter cold of the night covers the small streams of the Puna with a thin layer of ice, which had not yet melted in the early morning when the photograph was taken. - Book: Picture 160 - Chile - 1976

Rock paintings at Taira on the Río Loa in the Atacama Desert, northern Chile. These engraved and painted depictions of llamas are attributed to the Neolithic Atacameños. - Book: Picture 41 - Chile - 1976

Pucará de Lasana, an abandoned Atacameño village on the Río Loa in the Atacama Desert, Chile. The Atacameños practised terraced farming with artificial irrigation and built their dwellings close together so as not to waste the barren arable land. - Book: Picture 53 - Chile - 1976

As a high-altitude, cold desert, the Puna de Atacama is one of the most inhospitable regions on Earth. Bare rock and sand, lava flows and volcanoes characterise this forbidding yet impressive landscape. - Book: Picture 161 - Chile - 1976

The El Tatio geyser field in the Atacama Desert in northern Chile, situated at an altitude of around 4,200 metres. It is one of the highest geyser fields in the world. Activity is at its peak in the early morning (between 6.00 and 8.00 am), as this is when the temperature differences are greatest and the steam from the geysers rises most vigorously. The volcano in the background is the dormant stratovolcano Tatio (5,198 m). It lies directly on the border between Chile and Bolivia and forms part of the larger Tocorpuri volcanic complex. The name Tatio comes from the ancient Kunza language (Tata-iu) and translates as ‘the weeping grandfather’. It refers to the shape of the mountain range, which, from a distance, resembles the profile of an elderly man lying down. – Chile – 1976

An active geyser with a large fountain of steam in the El Tatio geothermal area in the Chilean Andes, at an altitude of around 4,280 metres in the Antofagasta Region. The best time to visit is early in the morning, when the fountains and steam are particularly impressive in the cold early-morning temperatures. – Chile – 1976

The rhyolite lava flows in the Chilean Puna de Atacama are associated with major tectonic fault lines striking in a north-south direction. The Tatio geysers, whose hot water vapour condenses in the cold high-altitude air, provide evidence that magmatic flow is present at shallow depths. It is rainwater that has seeped into the ground, heated up at depth and, due to the resulting pressure, is ejected either continuously or at regular intervals. - Book: Picture 162 - Chile - 1976

The impressive El Tatio geyser field is one of the highest and largest in the world, featuring numerous hot springs, fumaroles and rising columns of steam. Due to the extreme altitude (4,280 m) and the cold mountain air, the temperature difference between the hot water and the surrounding environment is particularly evident in the large clouds of steam in the morning. – Chile – 1976

The photograph shows the El Tatio geothermal field in the Andes in northern Chile, which lies at an altitude of around 4,280 metres and is one of the highest in the world. It is situated approximately 80 km north of San Pedro de Atacama. Over 80 active geysers spout large clouds of steam into the cold desert air, particularly in the early hours of the morning. – Chile – 1976