Posted by chris in suburbia on September 27, 2005 at 17:39:28:
From an email from SCEC....chris SCEC News is pleased to announce another free USGS Public Lecture to be held on Thursday, September 29th at 8pm. Dr. Mary Lou Zoback of the USGS Menlo Park office will present "The 1906 Earthquake: Lessons Learned and Lessons Forgotten." A synopsis is given below. Please join the USGS Pasadena office for the fifth year of their Public Lecture Series! All lectures are free and begin at 8 pm in Beckman Institute Auditorium on the Caltech campus in Pasadena. There is plenty of free parking available.
For more information see http://pasadena.wr.usgs.gov/info/lectures/ or call 626-583-6801.
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The 1906 Mw7.8 earthquake on the northern San Andreas Fault marked the birth of modern earthquake science. For the first time, the effects and impacts of a major seismic event were systematically investigated and documented in a detailed report. Scientists not only carefully mapped the entire 200-mile-long fault rupture, but they also mapped the fault south to the Mexican border, showing the San Andreas as a major geologic structure for the first time. They showed that the strongest shaking occurred in areas of "made land" (fill) and soft sediment including China Basin and the present day Marina district -- two San Francisco neighborhoods heavily damaged again in 1989 during the Loma Prieta earthquake. Their surveys of damage to structures concluded that destruction was closely related to building design and construction -- a painful lesson oft repeated around the world. Perhaps the most important scientific result to come out of the 1906 earthquake was the concept of an earthquake cycle. As earthquake science evolves, reanalysis of the 1906 earthquake data continues to yield new insights about that event and the behavior of large strike-slip faults in general. Looking to the future, a dense array of continuous GPS recorders in N. California, part of EarthScope's Plate Boundary Observatory, can search for fault interactions and determine if an acceleration of strain rate precedes the next big earthquake as it may have prior to 1906. Come and find out how we are still learning from "the big one" that happened 100 years ago!
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