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Elevation map of the study area

Elevation map of the study area

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Ecological processes such as landslide disaster are primarily impacted by both geological and land use activities happening at different spatiotemporal scale. They specifically impact the socioeconomic development in the sub-Himalayan region of Pakistan. Ecological risk assessment and restrictive zonation mapping are therefore prerequisites for mit...

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... i.e., topographic factors, physical factors and anthropogenic factors. Topographic factors included tilt direction, slope angle, and elevation. These factors were derived from the Shuttle Radar Topography Mission (STRM) Digital Elevation Model (DEM) of 30 m resolution. Area under study fell in the elevation range of 437 to 2053 m as shown in Fig. 4. Ten classes of Tilt direction were created, i.e., flat (-1), north (0-22.5), northeast (22.5-67.5), east (67.5-112.5), southeast (112.5-157.5), south (157.5-202.5), southwest (202.5-247.5), west (247.5-292.5), northwest (292.5-337.5), north (337.5-360) ( Fig. 5), whereas slope angle was divided into five intervals, i.e., 0°-45°, ...

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... Their study in South Korea analyzed causative factors such as slope angle, altitude, soil texture, and forest density, validating our use of high-weighted factors particularly slope degree and lithology in assessing landslide hazard. Similarly, Saleem et al. (2020) highlighted that slope degree, lithology, land use/land cover, and precipitation are among the most influential factors for landslide susceptibility in the sub-Himalayan region, further confirming our results. In the context of flood hazard assessment, Dung et al. (2022) provided a comprehensive review of flood hazard zoning using AHP. ...
... Bioengineering techniques, such as planting deep-rooted vegetation, can further reinforce slopes and reduce erosion. This approach has been effective in landslide-prone regions of the Himalayas, where vegetation has been used to stabilize slopes and prevent soil erosion (Saleem et al. 2020). ...
... Participatory planning, which involves local communities in the development and implementation of risk mitigation strategies, can also improve the effectiveness and sustainability of these measures. This approach has been successfully applied in the sub-Himalayan region, where community input has led to more effective landslide mitigation strategies (Saleem et al. 2020). ...
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... Zhou et al. [8] calculated the landslide hazard and vulnerability of the region based on the contribution weight model and used GIS technology to overlay the two to obtain the geological disaster risk zoning. Saleem et al. [9] used an analytical hierarchical process (AHP) to assign weights to the susceptibility factors of landslides in the sub-Himalayan region of Pakistan and obtained susceptibility zones using the weighted overlay method. Liu et al. [10] considered various factors that influenced landslide occurrence and used AHP combined with GIS technology to assess landslide susceptibility in the region. ...
... When using the failure value F D obtained from Equation (9) as the possibility of landslide occurrence, if the calculated failure value of the slope corresponds to the natural state, no conversion is required. If the calculated failure value of the slope results from the action of rainfall or an earthquake, it is necessary to consider the recurrence period of the rainfall or earthquake necessary, and the failure value calculated using Equation (9) should be divided by the return period to obtain the annual failure value of the slope [42]. where is the symbolic function. ...
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