A geomorphological approach to the estimation of landslide hazards and risks in Umbria, Central Italy

Abstract

Abstract. We present a geomorphological method to evaluate landslide hazard and risk. The method is based on the recognition of existing and past landslides, on the scrutiny of the local geological and morphological setting, and on the study of site-specific and historical information on past landslide events. For each study area a multi-temporal landslide inventory map has been prepared through the interpretation of various sets of stereoscopic aerial photographs taken over the period 1941-1999, field mapping carried out in the years 2000 and 2001, and the critical review of site-specific investigations completed to solve local instability problems. The multi-temporal landslide map portrays the distribution of the existing and past landslides and their observed changes over a period of about 60 years. Changes in the distribution and pattern of landslides allow one to infer the possible evolution of slopes, the most probable type of failures, and their expected frequency of occurrence and intensity. This information is used to evaluate landslide hazard, and to estimate the associated risk. The methodology is not straightforward and requires experienced geomorphologists, trained in the recognition and analysis of slope processes. Levels of landslide hazard and risk are expressed using an index that conveys, in a simple and compact format, information on the landslide frequency, the landslide intensity, and the likely damage caused by the expected failure. The methodology was tested in 79 towns, villages, and individual dwellings in the Umbria Region of central Italy.

Tree-Ring Reconstruction of Debris-Flow Events Leading to Overbank Sedimentation on the Illgraben Cone (Valais Alps, Switzerland)

“…In inhabited areas, they may cause damage to transportation corridors and buildings or even lead to the loss of lives [1,2]. As a consequen-ce, the understanding of the process as well as the behavior of debris-flow events in space and time is crucial for the mitigation of related hazards and risks [3][4][5].…”

Mapeamento da Fragilidade Ambiental na Bacia do Rio Aldeia Velha, RJ

“…Nessa perspectiva, modelos qualitativos empíricos são empregados na análise da fragilidade ambiental para avaliação do fenômeno da erosão, no que diz respeito a sua origem, evolução e condicionantes, podendo fundamentar-se na experiência de especialistas (Kappes et al, 2012;Cardinali et al, 2002).…”

Risk-based analysis of monitoring time intervals for landslide prevention

“…in the study region to estimate landslide occurrence frequency. The lack of landslide occurrence information and the difficulty of achieving a complete or systematic landslide record from the past have been demonstrated in previous research (Jaiswal et al, 2010;van Westen et al, 2006;Cardinali et al, 2002). From the previous studies, methods to estimate landslide frequency from the available information were summarized as five schemes: observation experience at a site, inventories from landslide statistics, triggering event equating, cause and effect model from geomorphology, and deterministic stability model (A. G. S., 5 2000).…”