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The scientists in this study refined a new method that uses the amount of sediment that collapses off of a fault scarp to estimate the fault offset at that location. Two or more of the paleoearthquakes appear to have ruptured across the boundary between the Provo and Salt Lake City segments, but further studies are needed to confirm.
A close-up view of the Salt Lake City and Provo segments of the Wasatch fault zone, indicated by the white rectangle in map a. The two trench sites yellow stars from these studies are located on either side of the boundary between these two fault segments. The small black and white arrows highlight the top and bottom of the fault scarp, respectively.
The black line across trench shows the location of the Wasatch fault, where it juxtaposes different color geologic units tan and brown. At the Corner Canyon site, the scientists also found geologic evidence of six ground-rupturing earthquakes on the southernmost part of the Salt Lake City segment in the past years. For this study, the scientists developed a multiple-method approach to evaluate and model the timing of individual earthquakes at the site.
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Paleoseismologists typically analyze collected data using statistical analysis, which works well in a geological environment where earthquakes occur among a continuous and uninterrupted sedimentary record, such as in lakes or ponds. The new multi-method approach developed in this study more accurately assesses earthquake timing in areas with a more sporadic sedimentary record. Collectively, the results from these two fault-trench studies demonstrate the history of large earthquakes on either side of the boundary between Salt Lake City and Provo segments.
The results also refined and confirmed two new data analyzation methods for complex geologic environments along with an active fault zone. These data will help fill in the complex puzzle of what is going on along the Wasatch fault zone and what we might expect to happen during the next large earthquake along the Wasatch Front.
The newly developed methods will be used to reanalyze all previous paleoseismic data for this part of the Wasatch fault zone, to evaluate whether past earthquakes have ruptured more than one fault segment at the same time. Maps of the Corner Canyon site showing a an overview of the area and b a close-up view of the rectangular area shown in map a with the trench drawn in as a rectangle and dashed line.
A photo from the Alpine site showing the extent of the trench across the Wasatch fault white arrows , as well as the top and bottom of the scarp caused by vertical offset from past earthquakes.
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A photo of one exposed wall of the Alpine trench showing the Wasatch fault and the sense of motion on the fault red lines and arrows. The alluvial fan deposits are shown by the dashed white lines. Christopher B. DuRoss, Scott E. Bennett, Richard W. Briggs, Stephen F. Personius, Ryan D. Gold, Nadine G. Reitman, Adam I. Hiscock, Shannon A. New releases. Add to Wishlist.
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