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
"Mediciones de espesor en glaciares de Chile centro-sur"
Rivera, A., Casassa. G., Acuña. C (2001) : “Mediciones de espesor en glaciares de Chile centro-sur” Revista Investigaciones Geográficas, 35: 67-100.
Resumen / Abstract.
The results of ice thickness measurements carried out in Chile (30-41°C) during recent years are presented. The information was obteined by means of radar in five glaciers. In all of therm, the radar signals were slightly attenuated allowing penetration of the ice to the bedrock. This means that the presence of supra, intra and subglacial meltwater did not affect the signals significantly. The system was tested on bare ice as well as debris covered ice. For debris covered ice areas, the signals were much more noisy than on bare ice, but they were able to penetrate the ice to the bedrock, obtaining a maximum thickness of 230 m in the ablation area of Juncal Norte glacier.
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