Andean Geology is becoming an English-language journal
This transition will be effective starting July 1, 2026. All submissions but obituaries and comments, and those part of special issues, will be required to be submitted in English
Call for Papers
Special Issue: Advances in Paleontology in Chile: Opportunities and Challenges for a Synthesis
Edited by:
- Marcelo Rivadeneira, CEAZA
- Enrique Bostelmann, Sernageomin
- Martín Chávez-Hoffmeister, CIAHN
- Joseline Manfroi, CIAHN
- Philippe Moisan, Universidad de Atacama
- Karen Moreno, Universidad Austral de Chile
- Sven Nielsen, Universidad Austral de Chile
- Ana Valenzuela-Toro, CIAHN
- Natalia Villavicencio, Universidad de O'Higgins
Submission status: Open between March 1, 2026, and November 30, 2026
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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 April 30, 2026
Instituto de Altos Estudios Espaciales Mario Gulich, Comisión Nacional de Actividades Espaciales (CONAE) y Universidad Nacional de Córdoba, Falda de Cañete, Ruta C45 km 8, 5187-Falda de Cañete, Córdoba, Argentina Argentina
Guillermo Toyos
Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET) based at Comisión Nacional de Actvidades Espaciales (CONAE), Buenos Aires, Argentina Argentina
Valérie Baumann
Institute of Earth Sciences (ISTE), Université Lausanne, Bâtiment Géopolis, 1015-Lausanne, Switzerland. Switzerland
On February 2009 intense rainfall triggered landslides in the Tartagal River basin that evolved into a debris flow that caused severe flooding in the town of Tartagal, Salta, Argentina. Based on these events, this paper presents a first attempt to map the landslides susceptibility in the Tartagal River basin. First, we elaborated an inventory map by using a 10 m pixel SPOT image acquired just after the disaster. Second, we evaluated a set of conditioning factors, which included lithology, slope and curvature; we derived the topographical variables from a 12.5 m pixel digital elevation model (DEM) based on a stereo-pair of satellite images ALOS-PRISM. Finally, we used these conditioning factors and the 2009 landslides inventory map as input for a heuristic model to elaborate the susceptibility map. The results indicated that landslides affected an area of 8 km2 and that at least 2.2x106 m3 of material were removed. The susceptibility map identified zones of low, moderate, high and very high susceptibility that occupied 18, 22, 25 and 17 km2, respectively. Accuracy assessment using data covering landslides occurred in 2006 showed that 95% of them fell within the high and very high susceptibility areas. The results presented herein provide vital baseline information for future studies and may contribute for the development of landslide hazard mitigation strategies.