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
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