3.8 Article

Soil Erosion and Landslide Susceptibility Mapping in Western Attica, Greece: A Rock Engineering System Approach

Journal

GEOSCIENCES
Volume 13, Issue 11, Pages -

Publisher

MDPI
DOI: 10.3390/geosciences13110338

Keywords

Mandra flash flood; soil erosion; slope failure; RES; mitigation measures; landslide susceptibility

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This article discusses the significant impacts of soil erosion and landslides on soil degradation, focusing on the case study of the Mandra flash flood in Greece. Through investigations and analyses, researchers developed soil erosion and landslide susceptibility maps and explored the relationship between them. The findings of this study could serve as a basis for modeling approaches in European landslide policies.
Two of the eight main soil degradation processes with which soils worldwide are confronted are soil erosion and landslides. Specifically, landslides are a major threat in particular areas across Europe, often leading to serious impacts on population, property, and infrastructure. Regarding the abovementioned processes, the case study of the fatal Mandra flash flood (November 2017) in the Attica Region (Greece), which caused 24 deaths, and much infrastructure and building damage, is presented with the intention of assessing the relationship between soil erosion and landslide incidents. Investigations were executed from 2018 to 2022, and their outcomes were taken into consideration by the Technical Authority of the Attica Region. Soil erosion lines were delineated in a GIS and were validated using a previously generated regional Web-GIS landslide susceptibility map. The study presents soil erosion types from the Mandra fatal flash flood event and correlates them with already existing landslide susceptibility analyses for the Attica Region. The produced susceptibility map is a cartographic product on a regional scale (1:100,000) generated via a semiquantitative heuristic methodology named the Rock Engineering System (RES). The way in which both soil erodibility and landslide susceptibility maps were generated and validated could be the basis for proposing modeling approaches that can respond to new developments in European landslide policies.

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