2022
DOI: 10.7494/geom.2022.16.2.77
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The Prevention of Landslides Using the Analytic Hierarchy Process (AHP) in a Geographic Information System (GIS) Environment in the Province of Larache, Morocco

Abstract: Landslides are one of the natural hazards that many countries around the world are facing. In Morocco, the Rif regions are the most affected by these phenomena. Each year they cause enormous damage to the road network and infrastructure, especially in our study region, the province of Larache.The study region is subject to several opening up and road construction projects, which is why it is necessary to predict and identify the most vulnerable areas beforehand, in order to propose measures and techniques whic… Show more

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Cited by 8 publications
(3 citation statements)
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“…phase: folds, thrust layers, overlaps, and fracturing [33,34]. In this area, a relatively calm structure is found, consisting of gray marls of the Upper Cretaceous (Senonian mainly), white marls and marl limestones from Eocene, and gray marls with sandstone banks of the Oligo-Miocene (sandstone "Larachian").…”
Section: Geological Context Of the Study Areamentioning
confidence: 98%
See 1 more Smart Citation
“…phase: folds, thrust layers, overlaps, and fracturing [33,34]. In this area, a relatively calm structure is found, consisting of gray marls of the Upper Cretaceous (Senonian mainly), white marls and marl limestones from Eocene, and gray marls with sandstone banks of the Oligo-Miocene (sandstone "Larachian").…”
Section: Geological Context Of the Study Areamentioning
confidence: 98%
“…From a geological point of view, the region of Ksar Kbir belongs to the basin of the lower Lokkous (Figure 2), which is located at the limit of the meso-Rifan zone and constitutes the entirety of its eastern and northeastern edge. The structuring of the region is part of the Alpine tectonic evolution that marks the Rif range, the dominant Meso-Cenozoic and Mio-Plio-Quaternary lands record the different structures that mark the major Alpine phase: folds, thrust layers, overlaps, and fracturing [33,34]. In this area, a relatively calm structure is found, consisting of gray marls of the Upper Cretaceous (Senonian mainly), white marls and marl limestones from Eocene, and gray marls with sandstone banks of the Oligo-Miocene (sandstone "Larachian").…”
Section: Geological Context Of the Study Areamentioning
confidence: 99%
“…For example, Hierarchical Fuzzy Inference Systems (HFIS) that were applied in the Rif Mountains' center region (Ozer et al, 2020) and fuzzy Analytical Hierarchy Process (FAHP) were combined for landslide susceptibility modeling in southeast Morocco (Sadiki et al, 2023); Weight Of Evidence (WOE) was applied in Tetouan-Ras Mazar (Elmoulat & Ait Brahim, 2018), an area of the Rif chain (Es-smairi et al, 2021) and Taounate-Ain Aicha . Logistic regression (LR) was used in Taounate-Oudka and the Sahla catchment area (El-Fengour et al, 2021), while the Analytical Hierarchical Processes (AHP) method was applied in Tangiers (Brahim et al, 2018), the Larache Province (Hamdouni et al, 2022) and parts of the Rif mountains (Es-smairi et al, 2021). However, these methods rely on assumptions about the data, such as normality and linearity, which can limit their accuracy in analyzing complex interrelationships between different causative factors.…”
Section: Introductionmentioning
confidence: 99%