For much of the twentieth century, seismologists operated on the principle that the gradual accumulation of strain along a fault line was the most reliable indicator of an impending earthquake's likely magnitude. The greater the strain buildup, the more violent the expected rupture. This conviction held until the 2004 Sumatra-Andaman earthquake, a massive event that originated on a fault segment where strain accumulation had been unremarkable. In the aftermath, a competing hypothesis gained ground: that the absolute level of stress already present in the crust, independent of its rate of increase, could be the decisive factor. The two views carry opposite implications for hazard assessment, since a region with slow strain accumulation might still be primed for a catastrophic release if absolute stress is high. A recent evaluation of eleven leading earthquake-forecasting models underscored the practical consequences of this theoretical split. When the models were asked to predict quake probabilities using only strain-rate data, their outputs clustered within a narrow range. Once absolute stress estimates were incorporated into the simulations, however, the forecasts scattered so widely that they became virtually useless for setting building codes or insurance premiums. The discrepancy leaves emergency planners in an untenable position: they must prepare for a worst-case scenario that existing models cannot even agree upon.
1. The author of the passage is primarily concerned withA. advocating for the superiority of one earthquake-forecasting approach over another
B. accounting for the unexpected severity of the 2004 Sumatra-Andaman earthquake
C. explaining why a once-dominant theory has been abandoned
D. detailing the practical difficulties that arise from unresolved scientific disagreement
E. comparing the methodologies employed by eleven different earthquake models
2. It can be inferred that one reason the eleven models described in the passage produced widely scattered forecasts when absolute stress estimates were included was thatA. absolute stress data are inherently less reliable than strain-rate measurements
B. the models were constructed using outdated information about fault mechanics
C. the researchers who built the models held differing views on how absolute stress influences earthquake likelihood
D. the models were designed to prioritize strain-rate data and could not properly integrate additional variables
E. the absolute stress levels varied so greatly from one fault to the next that no single model could account for all cases
3. The information in the passage suggests that emergency planners would be in a better position to set building codes if researchers could first answer which of the following questions?A. What is the maximum possible magnitude of an earthquake on a fault with slow strain accumulation?
B. Which of the two competing hypotheses—strain accumulation or absolute stress—is more consistent with the data from the 2004 Sumatra event?
C. How can strain-rate data be used to estimate absolute stress levels in the crust?
D. To what extent does the inclusion of absolute stress estimates alter the forecasts produced by a typical earthquake model?
E. What is the relative importance of strain accumulation versus absolute stress in determining the magnitude of an earthquake rupture?