Nine factors affecting landslide occurrences of the study area were used in the applied method. Each factor was divided into several classes which were further rate from zero to four representing different landslide hazard level. The Analytical Hierarchy Process (AHP) was combined with Geographical Information System (GIS) to support the evaluation and the calculation of weighting coefficient of the selected factors and to produce a landslide susceptibility assessment map. The influence of uncertainty of the factors’ weighting coefficient on the landslide susceptibility assessment results was examined and three scenarios were developed leading to the corresponding landslide susceptibility assessment maps. Finally, a landslide inventory map was generated and further used for the verification of the landslide susceptibility assessment map.
The results of the proposed method proved that the areas of very high and high landslide susceptibility are located mostly at the northern, western and southern part of the study area. These areas suffer from a large number of landslides mainly due to the prevailing geological and morphological conditions. The uncertainty analysis of the applied method showed insignificant differences on the spatial and quantitative distribution of the landslide susceptibility zones.
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...area comprises alpine and post alpine formations. The Alpine formations belong to two main stratigraphic zones, which are the Pindos zone and the Koziakas zone. The post-Alpine formations are molassic formations of the Mesohellenic trench, and Quaternary deposits, which cover the beds of rivers and streams. The study area is composed of: a) coarse grained loose to semi-coherent Quaternary deposits consisting of mainly of pebbles and gravels of varying sizes gravels, cones and scree, b) Miocene molassic clastic formations of Fanari series, c) flysch formations, which their main members are sandstones, siltstones and more rarely conglomerates, d) carbonate rocks consisting of Middle Triassic - Cretaceous limestones and e) Middle – Upper Jurassic clay – chert formations (IGME 1993).
The climate is Mediterranean with a rainy period that begins in October and ends in May.
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