Glaciares de Chile
- Glaciares del Volcán Melimoyu
- Glaciares del Nevado de Queulat
- Glaciares del Volcán Mentolat
- Glaciares del Volcán Cay
- Glaciares del Volcán Macá
- Glaciares del Volcán Hudson
- Glaciar Erasmo
- Glaciar San Rafael
- Glaciar San Quintín
- Campo de Hielo Norte
- Glaciar Nef
- Glaciar Colonia
- Lago Cachet II
- Glaciar Steffen
- Glaciares del Monte San Lorenzo
- Glaciar Jorge Montt
- Glaciar Lucía
- Glaciar Los Moscos
- Glaciar Bernardo
- Glaciar O’Higgins
- Glaciar Chico
- Campo de Hielo Sur
- Campo de Hielo Sur
- Glaciar Témpanos
- Glaciar Pío XI
- Glaciar Viedma
- Glaciar Perito Moreno
- Glaciar Dickson
- Glaciar Olvidado
- Glaciar Grey
- Glaciar Amalia
- Glaciar Pingo
- Glaciar Tyndall
- Glaciar Balmaceda
- Isla Desolación
- Glaciares de la Isla Santa Inés
- Seno Gabriel
- Glaciar Schiaparelli
- Glaciar Marinelli
- Fiordo Parry
- Cordillera Darwin
- Glaciar Garibaldi
- Glaciar Roncagli
- Glaciares Isla Hoste
Antártica
"Recent Fluctuations of Glaciar Pío XI, Patagonia: Discussion of a Glacial Surge Hypothesis"
Rivera, A., Aravena, J. & Casassa, G. (1997) : “Recent Fluctuations of Glaciar Pío XI, Patagonia: Discussion of a Glacial Surge Hypothesis” Mountain Research and Development, 17(4): 309-322.
Resumen / Abstract.
The Southern Patagonia Icefield remains one of the least studied glacial areas in the world, although it is one of the largest mid-latitude ice bodies. The largest glacier, Glaciar PíO XI, located on the western maritime side, has been advancing during the last 50 years. In 1993 the tidewater front of the glacier was overriding trees at least 300 years old.
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