A S Furumoto

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The seismic refraction traverses carried out for the project are shown in Figures 1,2, and 3. Figure 1 shows the traverses designated by code 1 Hawaii Institute of Geophysics Contribution No. 90. THE ISLAND OF OAHU in the Hawaiian ArchiINSTRUMENTATION pelago was formed by the coalescing of two Because mobility was necessary for the planned volcanoes,(More)
Seismic studies using well-logging, refraction, and reflection methods were carried out in 1965 in conjunction with a core-sample drilling project in the Ewa Coastal Plain, Oahu, Hawaii. The seismic well-logging technique gave a complicated velocity-depth profile, with higher velocities associated with reef limestone and lower velocities associated with mud(More)
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