Statistical analysis of Landslide in South district, Sikkim, India: using Remote Sensing and GIS

Landslides are among the most costly and damaging natural hazards in mountainous region, triggered mainly under the influence of earthquakes and/or rainfall. In the present study, Landslide Hazard Zonation (LHZ) of South district, Sikkim State was carried out using Remote Sensing and Geographic Information System (GIS). Various thematic layers namely slope, photo-lineament buffer, thrust buffer, relative relief map, geology and land use / land cover map were generated using remote sensing data and GIS. The weighting rating system based on the relative importance of various causative factors as derived from remotely sensed data and other thematic maps were used for the LHZ. The different classes of thematic layers were assigned the corresponding rating value as attribute information in the GIS and an ‘‘attribute map’’ was generated for each data layer. Each class within a thematic layer was assigned an ordinal rating from 0 to 9. Summation of these attribute maps were then multiplied by the corresponding weights to yield the Landslide Hazard Index (LHI) for each cell. Using trial and error method the weight-rating values have been re-adjusted. A LHZ map was prepared showing the five zones, namely ‘‘very low hazard’’, ‘‘low hazard’’, ‘‘moderate hazard’’, ‘‘high hazard’’ and ‘‘very high hazard’’ by using the ‘‘slicing’’ operation.

[1]  P. DeCelles,et al.  Implications of shortening in the Himalayan fold‐thrust belt for uplift of the Tibetan Plateau , 2001 .

[2]  V. Joshi,et al.  Control measures for soil erosion, landslides and debris flow in Hindu-Kush Himalayan belt of People's Republic of China. , 2000 .

[3]  Kei Sato,et al.  Anatomy of a Cambrian suture in Gondwana: Pacific-type orogeny in southern India? , 2009 .

[4]  S. Schumm EVOLUTION OF DRAINAGE SYSTEMS AND SLOPES IN BADLANDS AT PERTH AMBOY, NEW JERSEY , 1956 .

[5]  Jan Otto Larsen,et al.  Landslide hazards and mitigation measures at Gangtok, Sikkim Himalaya , 2002 .

[6]  M. Santosh,et al.  CO2 windows from mantle to atmosphere: Models on ultrahigh-temperature metamorphism and speculations on the link with melting of snowball Earth , 2008 .

[7]  Sumit Ray Lateral variation in geometry of thrust planes and its significance, as studied in the Shumar allochthon, Lesser Himalayas, eastern Bhutan , 1995 .

[8]  D. Rowley Age of initiation of collision between India and Asia: A review of stratigraphic data , 1996 .

[9]  Varun Joshi,et al.  Landslide movement monitoring using GPS technology: A case study of Bakthang landslide, Gangtok, East Sikkim, India , 2011 .

[10]  D. K. Agrawal Perspectives of mountain risk engineering in the Himalayan Region , 1997 .

[11]  Debi Prasanna Kanungo,et al.  Terrain Analysis and Spatial Assessment of Landslide Hazards in Parts of Sikkim Himalaya , 1996 .

[12]  Gautam Mitra,et al.  Thrust geometries and deep structure of the outer and lesser Himalaya, Kumaon and Garhwal (India): Implications for evolution of the Himalayan fold‐and‐thrust belt , 1994 .

[13]  R. Soeters,et al.  Digital geomorphological landslide hazard mapping of the Alpago area, Italy , 2000 .

[14]  R. Horton Drainage‐basin characteristics , 1932 .

[15]  K. Valdiya Geology of Kumaun Lesser Himalaya , 1980 .

[16]  A. Gansser Geology of the Himalayas , 1964 .