Seismic Hazard of the Uttarakhand Himalaya, India, from Deterministic Modeling of Possible Rupture Planes in the Area

<table>Simulated acceleration records at Gopeshwar station for parameters of the Chamoli earthquake on 29 March, 1999, by considering all possibilities of nucleation point within the rupture plane. The shaded rectangle shows the nucleation point which gives maximum ground acceleration.</table>

International Journal of Geophysics

fig7

Figure 7

Figure 7: Seismic Hazard of the Uttarakhand Himalaya, India, from Deterministic Modeling of Possible Rupture Planes in the Area 