I. The distribution of tsunami amplitudes in the open ocean is controlled by source mechanism and bathymetry geometry. Although detailed studies have considered heterogeneity effects in earthquake tsunami sources, little or no attention has been paid to the effects of physical resolution of detailed bathymetry on tsunami waveforms in the...
The structure of the North American crust and mantle was investigated using P wave teleseismic tomography and the links between seismic tomographic models, locations of volcanism, sediment isopachs, and continental scale crustal structures via plate reconstruction modeling. Nearly 50,000 teleseismic P wave delay times were measured from seismograms recorded by...
Despite advancing knowledge about the mechanics of earthquakes, earthquake prediction remains, and will likely remain, an unsolved problem. Hence in order to reduce the risk posed by earthquake shaking, seismologists have developed tools called earthquake hazard maps. Earthquake hazard maps communicate expected future shaking scenarios, and are used by engineers...