14. Penitentes
Location: On very high-altitude glaciers, such as those in the Andes mountain, where the air is dry.
These marvelous structures are tall thin blades of hardened snow or ice closely spaced with the blades oriented towards the general direction of the sun. They usually formed in clusters and range from a few centimetres to 2 meters but penitentes as high as 5 meters has been recorded. These pinnacles of snow or ice grow over all glaciated and snow covered areas in the Dry Andes above 4,000 meters. Penitentes are a common sight in the regions between Argentina and Chile. They form when the sun’s rays turn snow directly into water vapor without melting it first, a process called sublimation. An initially smooth snow surface first develops depressions as some regions randomly sublimate faster than others. The curved surfaces then concentrate sunlight and speed up sublimation in the depressions, leaving the higher points behind as forests of towering spikes.