1. Introduction
Landslide incidences in Himalayan region are about 30% of the total number of landslides in the world. Landslide damages the economic status, properties and also losses of lives all over the world [1]. Landslides are caused by meteorological, topographical, geo-environmental and geological factors and due to anthropogenic actions such as road constructions, open-pit mining, power house excavations, and land-use pattern changes [2]. Natural reasons of landslides consist of glacier melting, precipitation and earthquakes etc. Presently, the landslides phenomenon increased drastically due to impact of climate changes [3]. These factors motivated for thorough investigation and development of effective techniques for the susceptibility mapping. The present study focuses on the Uttarakhand, a state of India. From the survey reports, it is found that in 1998, more than 150 people were died due to landslide and a number of villages were affected in the state and more than 4000 causalities were recorded in June 2013 [4]. Landslide susceptibility map (LSM) is considered as an essential measure of landslide management of a landslide prone region [5]. LSMs could be implemented for minimizing effect of landslide on human kind, infrastructures, road networks, and land-use management [6]. Landslide susceptibility is defined as the probability of landslide occurrences by considering previous cases under the analogous geo-environmental conditions [7]. There are numerous techniques assisted by Geographic Information System (GIS) and Remote Sensing techniques that have been extensively used to generate LSMs by many researchers.