Geotechnical lessons from the Mw 7.1 2018 Anchorage Alaska earthquake

Author:

Cabas Ashly1,Beyzaei Christine2,Stuedlein Armin3,Franke Kevin W4,Koehler Richard5,Zimmaro Paolo67,Wood Clinton8,Christie Samuel9,Yang Zhaohui10,Lorenzo-Velazquez Cristina1

Affiliation:

1. North Carolina State University, Raleigh, NC, USA

2. Exponent, Oakland, CA, USA

3. Oregon State University, Corvallis, OR, USA

4. Brigham Young University, Provo, UT, USA

5. Nevada Bureau of Mines and Geology, University of Nevada, Reno, NV, USA

6. Department of Environmental Engineering, University of Calabria, Rende, Italy

7. Department of Civil and Environmental Engineering, University of California, Los Angeles, Los Angeles, CA, USA

8. University of Arkansas, Fayetteville, AR, USA

9. Kleinfelder, Redmond, WA, USA

10. University of Alaska Anchorage, Anchorage, AK, USA

Abstract

The 2018 Mw 7.1 Anchorage, Alaska, earthquake is one of the largest earthquakes to strike near a major US city since the 1994 Northridge earthquake. The significance of this event motivated reconnaissance efforts to thoroughly document damage to the built environment. This article presents the spatial variability of ground motion intensity and its correlation with subsurface conditions in Anchorage, the identification of liquefaction triggering in the absence of surficial manifestations (such as sand boils or sediment ejecta), cyclic softening failure in organic soils, and the poor performance of anthropogenic fills subjected to cyclic loading. In addition to lessons from observed ground deformation and geotechnical effects on structures, this article provides case studies documenting the satisfactory behavior of improved ground subjected to cyclic loading and the appropriateness of current design procedures for the estimation of seismically induced sliding displacements of mechanically stabilized earth walls.

Funder

national science foundation

Publisher

SAGE Publications

Subject

Geophysics,Geotechnical Engineering and Engineering Geology

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