Handbook of Hydroinformatics 2023
DOI: 10.1016/b978-0-12-821961-4.00003-8
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Identification of soil erosion sites in semiarid zones: Using GIS, remote sensing, and PAP/RAC model

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Cited by 6 publications
(6 citation statements)
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“…This entire area has been subjected to low-intensity regional metamorphism. Above these deposits to the north, we found the Paleozoic (Cambrian-Ordovician) lithological units, characterized by sandstone and schist facies, which are predominantly overlain by Mesozoic limestone carbonates (Jurassic and Cretaceous), as described by Diani et al [58]. The Toudgha River path is surrounded by Tertiary formations, mainly consisting of carbonates that are consolidated limestone and soft to poorly consolidated white-to-purplish sandstone.…”
Section: Study Areasupporting
confidence: 75%
See 1 more Smart Citation
“…This entire area has been subjected to low-intensity regional metamorphism. Above these deposits to the north, we found the Paleozoic (Cambrian-Ordovician) lithological units, characterized by sandstone and schist facies, which are predominantly overlain by Mesozoic limestone carbonates (Jurassic and Cretaceous), as described by Diani et al [58]. The Toudgha River path is surrounded by Tertiary formations, mainly consisting of carbonates that are consolidated limestone and soft to poorly consolidated white-to-purplish sandstone.…”
Section: Study Areasupporting
confidence: 75%
“…It is bordered to the north by the Central High Atlas Mountains and to the south by the Anti-Atlas Mountains chain. The Toudgha River is the main tributary in The Toudgha river catchment is located in the western region of the large Ziz-Ghris basin, which is a tectonic depression formed during the Mesozoic era as described by Diani et al [58]. It is bordered to the north by the Central High Atlas Mountains and to the south by the Anti-Atlas Mountains chain.…”
Section: Study Areamentioning
confidence: 99%
“…Previous studies have shown the importance of qualitative and holistic assessment methods for erosion prediction in risk mitigation measures in North African landscapes [32,33]. The qualitative method differs from the quantitative method in that it assigns weights to geographical units corresponding to soil erosion intensity [34]. The qualitative and quantitative models consider the same erosion factors, such as land use and land cover, soil type, slope gradient, and precipitation [35].…”
Section: Introductionmentioning
confidence: 99%
“…Our current understanding of erosion rates in semi‐arid to arid settings owing to overland flow and gully erosion is still limited, despite significant advances in recent years (Armoza‐Zvuloni et al, 2022; Diani et al, 2023; Mor‐Mussery & Laronne, 2020). One of the main challenges in evaluating erosion rates in these regions is the variability of the landscape and the complexity of the erosion processes (de la Torre‐Robles et al, 2023; García‐Ruiz et al, 2013; Gourfi et al, 2020).…”
Section: Introductionmentioning
confidence: 99%