Fractal investigation is a valuable technique to model and quantify the composite patterns of natural similarobjects. This study investigates Neotectonics using ASTER-GDEM. Fractal technique for extraction of topographicfractal dimension (Dtopo) and vertical dissection (Rtopo-surf) were used to assess the Neotectonics deformation.Geomorphological regions can be demarcated by using above mentioned procedures as they reveal the topographicevolutionary stages as an evaluation of topographic textures. The idea is to recognize the zones that are stronglyinfluenced by Neotectonics. Astore-Deosai-Skardu (ADS) region in Gilgit-Baltistan was selected for this purpose as itlies between MKT and MMT which is experiencing surface topographic deformation (STD) caused by anti-clock-wiseprogression and subduction of Indian plate beneath Eurasia. The results obtained illustrates that Dtopo and Rtopo-surf showanomalies in the ADS region that clearly represent a robust control of nearby MMT, MKT and KkF and highlights theirsignificance to describe regions vulnerable to Neotectonics and related deadly events threatening precious human livesand infrastructure damages.