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Natural or man‐made disasters are dreadful incidents that devastate lives, disturb the socioeconomic and socio-political structure of a society and preserve or erase developments and gains based on decades, within few minutes. A catastrophe has the capacity to affect existing general population to their base, parting an occasion for self-investigation and reassessment of their framework and composition. This study signifies the Radar Digital Elevation Model centered pattern of drainage network to appraise the catastrophic landslide events due to the 2005 earthquake in Neelum-Jhelum Valley in SE-Indus Kohistan Zone north of Pakistan. This investigation highlights zones affected by the earthquake and vulnerable to landslides by utilizing Hypsometric integrals (HI values) and Hack SL-gradient techniques that are proficient in detecting erosion, land mass and tectonic movements. Dataset principally includes “Shuttle Radar Topography Mission (SRTM)” Digital Elevation Model having pixel resolution of 90 meters. Hypsometric investigation brings evidence related to the deformation periods of a geographical stage. To accomplish this objective, D8 method was used, 355 subbasins of 4th Strahler order, from 5th Strahler order 75 subbasins and from 6th Strahler order 15 subbasins were delineated. To appraise the indentations of erosional scarps, Hypsometric curves (HC) and Hypsometric integrals (HI) for all distinct subbasins were computed. Variable topographic elevations (Maximun, minimum and mean) were determined to decipher the HI values. The HCs are characterized as convex up, S shaped and concave down curves. Curvature of convex up symbolizes a lesser amount of eroded or deformed subbasins (comparatively young geography), and are located in conjunction of the North-Eastern anticline side of the Muzaffarabad that indicates the tectonic behavior of HKS, however S-shaped curvatures denote the transitional stage between the convex up and concave down deformational stage. The curvatures of concave down represents extreme deformation phase and are located west and eastern side of HKS.