Ground Deformations Observed After 23.10.2011 Mw 7.2 VAN Earthquake (Turkey)

Publication Year:
2013
Usage 23
Downloads 16
Abstract Views 7
Repository URL:
http://scholarsmine.mst.edu/icchge/7icchge/session04/12
Author(s):
Akin, Mutluhan; Ozvan, Ali; Akin, Muge K.; Topal, Tamer
Publisher(s):
Missouri University of Science and Technology
Tags:
Geotechnical Engineering
conference paper description
A destructive earthquake with a moment magnitude of 7.2 occurred in the north of the Van province (Turkey) on 23rd October 2011 at 13:41 local time and caused approximately 600 deaths and more than 4000 injuries. Many damaging aftershocks were recorded for more than a month after the main shock including a triggered earthquake (Mw 5.6) located in the southern district of Van, namely Edremit, on November 9th, 2011 which caused additional damage and casualties. After the Mw 7.2 Van earthquake, earthquake-induced ground deformations such as liquefaction and lateral spreading were extensively observed around the shores of Lake Van and in the floodplains of rivers. The Karasu River floodplain, which is one of the major streams in the region, severely suffered from liquefaction and lateral spreading. In this study, a brief overview of the Mw 7.2 Van earthquake as well as earthquake-induced ground deformations is presented. Then, the results of field reconnaissance on liquefaction and lateral spreading features observed in the Karasu River floodplain are explained. Furthermore, subsurface characteristics of liquefied layers are documented considering the data obtained from a borehole drilled just on top of the sand boil after the earthquake. The borehole data indicate that the liquefaction occurred in a sandy zone with very shallow groundwater level in the Karasu River floodplain.