The northeastern part of the Indian subcontinent, considered as the most
active seismic zone of the Indian subcontinent, was hit by an earthquake of
Mw 5.6 on January 3, 2017. The epicenter of this earthquake was Kanchanbari
located in the Dhalai district of Tripura. The present study aims to assess
the environmental and socio-economic impact of this earthquake in the
vicinity of the epicenter. To assess and determine the level of damage, the
affected areas were visited during the first week of the 2017 earthquake.
Various Government offices were also consulted to acquire data on damages
caused by the earthquake. Moreover, Remote Sensing and Geographical
Information System (RS & GIS) techniques were applied to address the
influence of this earthquake on bank erosion. During the field visit, the
striking features of soil liquefaction generated by the earthquake were
observed in the flood plain area of the Manu River. Landslide, with three
casualties in India and the neighbor Bangladesh, and damages of
infrastructure were also reported. Additionally, an assessment of the bank
erosion study revealed that the rate of the post-earthquake bank erosion
increased to 592%, compared to the pre-earthquake bank erosion within the
study length of the Manu River. The findings highlighted that the impact of
this earthquake is minimal. However, the seismotectonic features and
observation of the liquefaction within the risk zone of the earthquake
indicate a possible significant threat for the future.