![]() All these data and study indicates that the Kathmandu Valley sediments are dependent on the frequency of the seismic waves and the wave velocity is greater in the peripheral region than in the central part of the Valley. The results of both analysis methods were then compared to the amplitude of the Gorkha Earthquake and borehole data. About 20 data were recorded in each site and then shear wave velocity structure and graph of amplification ratio with their spatial distribution has been established with the help of software i.e. For this, five sites were selected such as Pulchowk, Chhauni, Gaushala, Buddhanagar and Bhainsepati. The present study was carried out to evaluate resonant frequency of the ground and to characterize subsurface ground based on shear wave velocity structure. Received: ApAccepted: Published: May 31, 2019 Central Department of Geology, Tribhuvan University, Kathmandu, Nepal ![]()
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