The role of the lithological setting on the landslide pattern and distribution

• Autor(a) principal: Henriques, Cristina
• Data de Publicação: 2015
• Outros Autores: Zêzere, José, Marques, Fernando
• Tipo de documento: Artigo
• Idioma: eng
• Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
• Texto Completo: http://hdl.handle.net/10451/28232
• topic: Landslides; Lithology; Predisposition; Validation

In landslide susceptibility mapping studies, the quality of whole inputs such as geological setting and DEM derivatives should be as high as possible. Given the strong relationship between landslide occurrences and geology the use of a detailed lithological map is certainly an alternative preferable to the most commonly available rough geological map. Therefore, this study focuses on this reality and proposes a procedure for improving the available geological map in a study area located 90 km North of Lisbon. Based on a 1:50,000 scaled official geological map and according to the litho-stratigraphic characteristics, the map improvement was performed using the interpretation of aerial photographs by stereoscopic analysis and further field validation. In order to assess the relevance of the lithological improvement regarding the relationships with landslide distribution, a comparison was performed between the results obtained with the official lithological map and the improved detailed lithological map using the Conditional Probability (CP), the Accountability (ACC) and Reliability (RLB) indexes. A landslide inventory, including shallow and deep-seated landslides, was prepared for the study area and landslideswere overlapped with both lithologicalmaps. The ACC and RLB indexes obtained with the detailed geological map are higher than equivalent features obtained with the official lithological map. From these procedures it was possible to conclude that the detailed lithological map has a better discriminating power than the official lithological map, enabling a better quality of the landslide susceptibility analysiswith the separation of the relevant lithological classes.