4.7 Article

Updating Inventory, Deformation, and Development Characteristics of Landslides in Hunza Valley, NW Karakoram, Pakistan by SBAS-InSAR

Journal

REMOTE SENSING
Volume 14, Issue 19, Pages -

Publisher

MDPI
DOI: 10.3390/rs14194907

Keywords

landslide; InSAR; landslide inventory; slope displacement; Hunza; Pakistan

Funding

  1. Second Tibetan Plateau Scientific Expedition and Research [SQ2021QZKK0201]
  2. important talent project of Gansu Province [2022RCXM033]
  3. National Natural Science Foundation of China [41661144046, 42007232]
  4. Science and Technology Planning Project of Gansu Province [18YF1WA114]
  5. Science and Technology Major Project of Gansu Province [19ZD2FA002]
  6. Fundamental Research Funds for the Central Universities [lzujbky-2021-ey05]

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Using SBAS-InSAR technology, this study detected ground surface deformation in the Hunza Valley and completed a comprehensive inventory of 118 landslides. The analysis of three large landslides revealed the characteristics and mechanisms of landslide development.
The Hunza Valley, in the northwestern Karakoram Mountains, North Pakistan, is a typical region with many towns and villages, and a dense population and is prone to landslides. The present study completed landslide identification, updating a comprehensive landslide inventory and analysis. First, the ground surface deformation was detected in the Hunza Valley by SBAS-InSAR from ascending and descending datasets, respectively. Then, the locations and boundaries were interpreted and delineated, and a comprehensive inventory of 118 landslides, including the 53 most recent InSAR identified active landslides and 65 landslides cited from the literature, was completed. This study firstly named all 118 landslides, considering the demand for globally intensive research and hazard mitigation. Finally, the deformation, spatial-topographic development, and distribution characteristics in the Hunza Valley scale and three large significant landslides were analyzed. Information on 72 reported landslides was used to construct an empirical power law relationship linking landslide area (A(L)) to volume (V-L) (V-L = 0.067 x A(L)(1.351)), and this formula predicted the volume of 118 landslides in this study. We discovered that the landslides from the literature, which were interpreted from optical images, had lower levels of velocity, area, elevation, and height. The SBAS-InSAR-detected active landslide was characterized by higher velocity, larger area, higher elevation, larger slope gradient, larger NDVI (normalized difference vegetation index), and greater height. The melting glacier water and rainfall infiltration from cracks on the landslide's upper part may promote the action of a push from gravity on the upper part. Simultaneously, the coupling of actions from river erosion and active tectonics could have an impact on the stability of the slope toe. The up-to-date comprehensive identification and understanding of the characteristics and mechanism of landslide development in this study provide a reference for the next step in landslide disaster prevention and risk assessment.

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