Mizuho Ishida Mizuno_Ishida
Period One: Profile Period Two:Notable Achievements Period Three: Impact on Our Lives
Period Four: Virtual Science Lab Ishida Top Page
 Period Three: Impact on Our Lives
How has your research actually benefited people?
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Speaking with Kobe high school students in 1997 about the Great Hanshin-Awaji Earthquake.
In 1978, the government passed a law that called for a stronger network for monitoring earthquake activity across the Tokai and Kanto districts. The National Institute for Earth Science and Disaster Prevention set about building a network to monitor seismic activity that might portend a major earthquake in this area.

Plates move at a rate of up to 10 centimeters a year. We drew up a series of cross-sections parallel to the movement of the plates--one for each 20-kilometer segment--and on these we plotted the focus of each tremor we recorded. In this way, we were able to show accurately how one plate slides under another. Previously, it had been supposed that the interface where the Philippine Sea Plate is sliding under the Pacific Plate was only 20 or 30 kilometers in width, but the Ishida model revealed that it was actually closer to 100 kilometers. What this meant was that the worst possible earthquake in the region was not in the range of magnitude 6, as previously thought, but in the range of magnitude 7. So, this research has made a great contribution to earthquake prediction as well as monitoring and disaster-prevention measures.
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With researchers at the International Seismological Center in Britain (1999).
The Great Hanshin Earthquake that devastated Kobe in 1995 spotlighted the importance of disaster prevention. Until then, we had poured most of our efforts into learning how to predict major quakes. But in the wake of the Kobe Earthquake, there emerged a new field called real-time seismology, which analyzes seismic waves right after a major earthquake hits for information on the scale of the quake and characteristics of the fault zone. The purpose is to calculate the intensity of the shaking that has occurred in various areas and gauge the level of damage that is likely to have occurred. This should help us target rescue efforts where they are most needed, to keep casualties to a minimum. I took office as chair of the Seismological Society of Japan directly after the Kobe quake, and I set up a committee to review new areas of research, including such topics as earthquake-resistant construction and disaster plans for local jurisdictions, with an eye to making seismology more relevant to people's lives.
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