Quantification of seismic activity is one of the most challenging problems faced by earthquake engineers in probabilistic seismic hazard analysis.Currently,this problem has been attempted using empirical approaches which are based on the regional earthquake recurrence relations from the available earthquake catalogue.However,at a specified site of engineering interest,these empirical models are associated with large number of uncertainties due to lack of sufficient data.Due to these uncertainties,engineers need to develop mechanistic models to quantify seismic activity.A wide range of techniques for modeling continental plates provides useful insights on the mechanics of plates and their seismic activity.Among the different continental plates,the Indian plate experiences diffused seismicity.In India,although Himalaya is regarded as a plate boundary and active region,the seismicity database indicates that there are other regions in the Indian shield reporting sporadic seismic activity.It is expected that mechanistic models of Indian plate,based on finite element method,simulate stress fields that quantify the seismic potential of active regions in India.This article explores the development of a finite element model for Indian plate by observing the simulated stress field for various boundary conditions,geological and rheological conditions.The study observes that the magnitude and direction of stresses in the plate is sensitive to these conditions.The numerical analysis of the models shows that the simulated stress field represents the active seismic zones in India. Quantification of seismic activity is one of the most challenging problems faced by earthquake engineers in probabilistic seismic hazard analysis. Current, this problem has been attempted using empirical approaches which are based on the regional earthquake recurrence relations from the available earthquake catalog. Hosted, at a specified site of engineering interest, these empirical models are associated with large number of uncertainties due to lack of sufficient data. Due to these uncertainties, engineers need to develop mechanistic models to quantify seismic activity. A wide range of techniques for modeling continental containers could be useful insights on the mechanics of plates and their seismic activity. Among the different continental plates, the Indian plate experiences diffused seismicity. In India, although Himalaya is considered as a plate boundary and active region, the seismicity database indicates that there are other regions in the Indian shield reporting sporadic seismic activity.I t is expected that mechanistic models of Indian plate, based on finite element method, simulate stress fields that quantify the seismic potential of active regions in India. This article explores the development of a finite element model for Indian plate by observing the simulated stress field for various boundary conditions, geological and rheological conditions. the study observes that the magnitude and direction of stresses in stresses in the plates is sensitive to these conditions. numerical analysis of the models shows that the simulated stress field represents the active seismic zones in India.