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Characteristic earthquake / Richter magnitude scale / Earthquake / Aftershock / Seismic hazard / Tsunami / Seismicity of the Sanriku coast / Seismology / Mechanics / Physics


Appendix F. Determining earthquake recurrence rates For each earthquake, a set of source parameters must be chosen that determines the initial condition for propagation modeling. Earthquake magnitude is the primary param
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Document Date: 2008-01-08 17:30:23


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City

Washington / D.C. / /

Company

W.R. S.P. / F4 Tsunami Pilot Study Working Group / Pacific Marine Environmental Laboratory / F5 F6 Tsunami Pilot Study Working Group / Furukawa / F1 F2 Tsunami Pilot Study Working Group / Nishenko S.P. / /

Continent

America / /

Country

Turkey / Japan / Chile / /

Event

Natural Disaster / /

Facility

Earthquake Research Institute / /

IndustryTerm

power-law distribution / tsunami energy / power-law exponent / power-law scaling relationship / /

Movie

A.D. / /

NaturalFeature

Cook Inlet / Gulf of Alaska / Sea of Marmara / /

Organization

American Geophysical Union / Seismological Society of America / National Earthquake Prediction Evaluation Council / National Oceanic and Atmospheric Administration / Geological Society / Earthquake Research Institute / /

Person

William Sound / /

Position

Time-predictable recurrence model for large earthquakes / Prince / General / /

Product

F-1a / /

ProvinceOrState

Alaska / Tokai / /

PublishedMedium

Geophysical Research Letters / Journal of Geophysical Research / /

Region

southern California / /

Technology

Geophysics / /

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