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Building Vulnerability to the 2008 Ilia-Achaia Earthquake Induced Slides
[chapter]
2013
Landslide Science and Practice
Macroseismic observations in the meizoseismal area of the Achaia-Ilia, Greece, M w 6.4 earthquake of 8 June, 2008, have shown that soil liquefaction occurred at a number of sites up to distances of 25 km from the causative fault. In one of these sites (SITE-I at coastal zone of Kato Achaia) the occurrence of liquefaction was extensive and was followed by lateral spreading. In another nearby site (SITE-II) only marginal liquefaction (or nonliquefaction) was observed. Following the macroseismic
doi:10.1007/978-3-642-31427-8_28
fatcat:awrpms7uibfc3mmtk55tcqqesa