Monitoring of Mountain Permafrost in the Central Andes, Cordon del Plata, Mendoza, Argentina
Sixty per cent of the Rio Blanco basin (54 km2), located between 32°54′ and 33°01′S and between 69°27′ and 69°15′W, in the Cordón del Plata, Frontal Cordillera, can be considered to be periglacial. The most important forms in the area are rock glaciers, two of which, Morenas Coloradas and El Salto,...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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Online Access: | https://doi.org/10.1002/(SICI)1099-1530(199701)8:13.0.CO;2-M |