Special Issue dedicated to Francisco Hervé: Global tectonic processes of the ancient southwestern Gondwana margin in South America and the Antarctic Peninsula
Edited by:
- Mauricio Calderón, PhD, Universidad del Desarrollo, Chile
- Paula Castillo, PhD, Universität Münster, Deutschland
- Robert Pankhurst, PhD ScD, United Kingdom
Submission status: Extended until September 30, 2025
Special Issue: Geoethics in Chile and Latin America - Contextual reflections for responsible geoscience
Edited by:
- Luisa Pinto, Universidad de Chile
- Hernán Bobadilla, Politecnico di Milano
- Tania Villaseñor, Pontificia Universidad Católica de Chile
- Pablo Ramírez, Universidad de Chile
- Millarca Valenzuela, Universidad Católica del Norte
Submission status: Open between August 15, 2025, and March 31, 2026
Departamento de Geología, Universidad de Chile, Plaza Ercilla 803, Santiago. Chile
Sergio A. Sepúlveda
Departamento de Geología, Universidad de Chile, Plaza Ercilla 803, Santiago.
Instituto de Ciencias de la Ingeniería, Universidad de O´Higgins, Libertador Bernardo O´Higgins 611, Rancagua. Chile
Constanza Celis
Departamento de Geología, Universidad de Chile, Plaza Ercilla 803, Santiago. Chile
Sofía Rebolledo
Departamento de Geología, Universidad de Chile, Plaza Ercilla 803, Santiago. Chile
Pablo Ceballos
Departamento de Geología, Universidad de Chile, Plaza Ercilla 803, Santiago. Chile
Landslide susceptibility maps of Santiago city Andean foothills, Chile
Marisol Lara, Sergio A. Sepúlveda, Constanza Celis, Sofía Rebolledo, Pablo Ceballos
Abstract
The urban expansion of Santiago city includes areas with geomorphological and geological conditions with potential to be affected by landslide processes. This work presents compiled landslide susceptibility maps for the Andean foothills of Santiago city, between Maipo and Mapocho rivers. The maps identify the areas prone to the generation of slides, falls and flows. The results show that the oriental foothills of Santiago city have moderate to high susceptibility of rock falls, rock and soil slides and debris flows. The most important of these landslide types are debris flows, due to the runout of this processes that may reach urban areas posing a risk for the city, for which detailed hazard studies are required.
Keywords
Landslides; Slides, Debris flows, Rock falls, Susceptibility