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
"Antecedentes Paleoambientales para el desarrollo sustentable de la Región de Antofagasta, Chile"
Romero, H and Rivera, A. (1998) : “Antecedentes Paleoambientales para el desarrollo sustentable de la Región de Antofagasta, Chile” Bamberger Geographische Schriften, 15: 335-349.
Resumen / Abstract.
The region of Antofagasta, located in the northernmost section of Chile is one of those apparently stable landscapes as a consequence of its desertic nature. However, its long term climatic variability has allowed the origin and evolution of several resources, like water, soils and vegetation, which in turn, has sustained the old and permanent settlement of local ethnias. Agriculture, pastoralim and mining have been the main economic activities.
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