Project Abstract
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In the past several years, geologists have presented new evidence that the Ventura and Pitas Point faults may ‘link together’ and rupture simultaneously in earthquakes far larger than had been previously believed. Because for much of their length, these faults lie under Santa Barbara Channel, a sizeable thrust event on this linked system could pose a serious and previously unrecognized hazard in the form of tsunami. In 2013 I have been modeling the tsunami and in-undation extent of various faulting scenarios that developed by the Ventura Special Fault Study Group as well as my own rupture scenarios that arise from applications of ‘ALLCAL–style’ physics-based earthquake simulations.
An adjunct effort of this proposal in 2013 dealt with earthquake simulators. A major accomplishment up-stepped from the existing ALLCAL2 fault system to one that represents the newly released UCERF3 fault system as closely as possible. The UCERF3 fault system consists of down dip width, strike, dip, rake, geological slip rate and surface traces of 313 fault sections. Surface traces consist of two endpoints and perhaps several points in-between. As provided however, the UCERF3 fault system is not suitable for earthquake simulation. Fact is, no unique way exists to adapt the UCERF3 fault system for earthquake simulation. Certain assumptions have to be made. Accordingly, I call my product UCERF3-ES to differentiate the two sets (ES referring to Earthquake Simulator). |