for damage to infrastructure that will happen during a great Hayward earthquake. Now that's customer service! Previous research by McFarland and Lienkaemper found this fault has stored up enough energy to produce a 6.8 magnitude earthquake. Created By: giftsbyruth. Born: October 13, 1925. Because prolonged afterslip can delay reconstruction of fault-damaged buildings and infrastructure, we analyzed its gradual decay to estimate when significant afterslip would likely end. Because a p-value of ~ 1 (logarithmic increase in displacement) was related to frictional afterslip (Marone et al. However, we expect its afterslip to last much longer than one year. a. cause irreversible brain damage. Which type of question is particularly problematic because they sometimes imply judgment and also invite defensiveness? Questions include the necessity of invoking the transient rheology and the relative importance of contributions from afterslip and viscoelastic relaxation. Scientists have discovered that the San Andreas Fault in California continued to slip for up to 12 years after the magnitude 6 Parkfield earthquake that hit the state in 2004. On: Jul 29, 2013. Start studying Psychology-Ch 20,21,22,23. ", It is impossible to tell when the Hayward Fault will rupture. Answer Save. In a study published in the Bulletin of the Seismological Society of America, geophysicist James Lienkaemper from the U.S. Geological Survey and Forrest McFarland of San Francisco State University, have now analyzed the Parkfield earthquake to create better afterslip forecasts for parts of the fault expected to rupture. Westward-directed postseismic seafloor displacements may be due flow via low-temperature, plastic creep within the lower half of a Pacific lithosphere weakened by plate bending. d. the UL for Vitamin B12 is set too high. Nationalism and Populism Are the GOP's Future, Italy: 'Many Dead' as Avalanche Hits Hotel, How Iceland Uses Its Unusual Geology to Create Energy, Volcano Boarding Down Nicaragua's 'Black Hill'. Report Jun 22, 2020 . Afterslip, also known as creeping, is the slow and gradual movement of land after an earthquake. ) or https:// means you’ve safely connected to the .gov website. Afterslip is the result of relaxation of a stress perturbation within the velocity-strengthening region, which arises when an earthquake propagates into that region from below. This forecasting of Napa afterslip suggests how we might approach the scientific and engineering challenges of afterslip from a much larger M~7 earthquake anticipated on the nearby, urban Hayward Fault. It's not clear at all. This postseismic deformation is due primarily to viscoelastic relaxation of stresses induced by the earthquake rupture and continuing slip (afterslip) or relocking of different parts of the fault. Author Profession: Leader. It can develop in both men and women, particularly in people who smoke, drink excessive amounts of alcohol, take steroid medication, or have a family history of hip fractures. An official website of the United States government. c. prevents folate from being converted to one of its active forms. Synonym Discussion of problematic. “[Hitler’s] vision . rec Afterslip is particularly problematic because: Marked out of 1.00 Find out more from Tom Broker and here F Flag https://www.google.com/amp/slucrtoday.ucr.edu/38678 amp queation Select one: . Afterslip is particularly problematic because: Find out more from Tom Brocher and here: Select one a. The two datasets are complimentary in determining the postseismic processes. Official websites use .gov The full afterslip model also requires significant slip (∼4 m) at or below 80 km depth. 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