Matches in SemOpenAlex for { <https://semopenalex.org/work/W2124403651> ?p ?o ?g. }
Showing items 1 to 77 of
77
with 100 items per page.
- W2124403651 endingPage "222" @default.
- W2124403651 startingPage "203" @default.
- W2124403651 abstract "Abstract The Farmington Siding landslide complex consists of liquefaction-induced landslides that show evidence of recurrent movement during Holocene and latest Pleistocene time. Features associated with the landslide complex indicate landsliding likely was triggered by strong ground shaking. Numerous faults active during the Holocene exist in the region, including the nearby Weber segment of the Wasatch fault zone. As part of a study to characterize the hazard associated with reactivated landsliding, I used a variety of independent techniques to evaluate the relative likelihood of earthquakes from different sources to trigger liquefaction-induced landsliding at the Farmington Siding landslide complex. Empirical earthquake magnitude-distance relations indicate landsliding could have been triggered by large earthquakes on any of the East Cache, West Cache, East Great Salt Lake, West Valley, Oquirrh, or Wasatch fault zones. Comparisons of peak horizontal ground accelerations with calculated critical accelerations, as well as quantitative estimates of liquefaction severity index and Newmark landslide displacements, illustrate the relative likelihood of liquefaction-induced landsliding caused by large earthquakes from these various sources. The results of these analyses indicate large earthquakes on the Weber segment are significantly more likely than earthquakes from other sources to trigger liquefaction-induced landsliding. Comparison of radiocarbon-based chronologies of landsliding and surface-faulting earthquakes shows a correspondence between the timing of large-scale liquefaction-induced landslides and earthquakes that coincide with relatively high Great Salt Lake levels. These results indicate the likelihood of future large-scale liquefaction-induced landsliding is not only closely tied to the likelihood of a surface-faulting earthquake on the Weber segment, but is further dependent on concurrent hydrogeologic conditions." @default.
- W2124403651 created "2016-06-24" @default.
- W2124403651 creator A5065641982 @default.
- W2124403651 date "1999-01-01" @default.
- W2124403651 modified "2023-09-24" @default.
- W2124403651 title "Comparative Evaluation of Earthquake Sources Associated with the Liquefaction-Induced Farmington Siding Landslide Complex, Northern Utah" @default.
- W2124403651 hasPublicationYear "1999" @default.
- W2124403651 type Work @default.
- W2124403651 sameAs 2124403651 @default.
- W2124403651 citedByCount "0" @default.
- W2124403651 crossrefType "journal-article" @default.
- W2124403651 hasAuthorship W2124403651A5065641982 @default.
- W2124403651 hasConcept C100134115 @default.
- W2124403651 hasConcept C121332964 @default.
- W2124403651 hasConcept C126691448 @default.
- W2124403651 hasConcept C127313418 @default.
- W2124403651 hasConcept C1276947 @default.
- W2124403651 hasConcept C140345934 @default.
- W2124403651 hasConcept C151730666 @default.
- W2124403651 hasConcept C165205528 @default.
- W2124403651 hasConcept C175551986 @default.
- W2124403651 hasConcept C186295008 @default.
- W2124403651 hasConcept C187320778 @default.
- W2124403651 hasConcept C191859794 @default.
- W2124403651 hasConcept C2524010 @default.
- W2124403651 hasConcept C33923547 @default.
- W2124403651 hasConcept C65865001 @default.
- W2124403651 hasConcept C83176761 @default.
- W2124403651 hasConcept C90987359 @default.
- W2124403651 hasConcept C99844830 @default.
- W2124403651 hasConceptScore W2124403651C100134115 @default.
- W2124403651 hasConceptScore W2124403651C121332964 @default.
- W2124403651 hasConceptScore W2124403651C126691448 @default.
- W2124403651 hasConceptScore W2124403651C127313418 @default.
- W2124403651 hasConceptScore W2124403651C1276947 @default.
- W2124403651 hasConceptScore W2124403651C140345934 @default.
- W2124403651 hasConceptScore W2124403651C151730666 @default.
- W2124403651 hasConceptScore W2124403651C165205528 @default.
- W2124403651 hasConceptScore W2124403651C175551986 @default.
- W2124403651 hasConceptScore W2124403651C186295008 @default.
- W2124403651 hasConceptScore W2124403651C187320778 @default.
- W2124403651 hasConceptScore W2124403651C191859794 @default.
- W2124403651 hasConceptScore W2124403651C2524010 @default.
- W2124403651 hasConceptScore W2124403651C33923547 @default.
- W2124403651 hasConceptScore W2124403651C65865001 @default.
- W2124403651 hasConceptScore W2124403651C83176761 @default.
- W2124403651 hasConceptScore W2124403651C90987359 @default.
- W2124403651 hasConceptScore W2124403651C99844830 @default.
- W2124403651 hasLocation W21244036511 @default.
- W2124403651 hasOpenAccess W2124403651 @default.
- W2124403651 hasPrimaryLocation W21244036511 @default.
- W2124403651 hasRelatedWork W1977350266 @default.
- W2124403651 hasRelatedWork W1978633116 @default.
- W2124403651 hasRelatedWork W1981493349 @default.
- W2124403651 hasRelatedWork W2090008930 @default.
- W2124403651 hasRelatedWork W2144907355 @default.
- W2124403651 hasRelatedWork W2259122242 @default.
- W2124403651 hasRelatedWork W2326651888 @default.
- W2124403651 hasRelatedWork W2354389381 @default.
- W2124403651 hasRelatedWork W2367405941 @default.
- W2124403651 hasRelatedWork W2380874312 @default.
- W2124403651 hasRelatedWork W2383695144 @default.
- W2124403651 hasRelatedWork W2523542214 @default.
- W2124403651 hasRelatedWork W2583542794 @default.
- W2124403651 hasRelatedWork W2726589658 @default.
- W2124403651 hasRelatedWork W2848672042 @default.
- W2124403651 hasRelatedWork W2900873193 @default.
- W2124403651 hasRelatedWork W2945443876 @default.
- W2124403651 hasRelatedWork W2970878624 @default.
- W2124403651 hasRelatedWork W2994942732 @default.
- W2124403651 hasRelatedWork W3197534887 @default.
- W2124403651 isParatext "false" @default.
- W2124403651 isRetracted "false" @default.
- W2124403651 magId "2124403651" @default.
- W2124403651 workType "article" @default.