“…Finding that 85% of sites without manifestation had LPI 45, Lee et al [35] concluded that LPI ¼ 13 was the OOP. Juang et al [32] first noted that the sites studied by Toprak and Holzer [54] were predominantly deposits of clean sands, while those examined by Lee et al [35] were mostly deposits of silty sands and sandy silts, postulating that the discrepancy in findings might be tied to fines-content. Papathanassiou [46] similarly evaluated LPI at sites with relatively high fines-content during the 1999 Chi-Chi (Taiwan), 1999 Kocaeli (Turkey), and 2003 Lefkada (Greece) earthquakes, and concluded that LPI¼19 was the OOP for the assessed dataset.…”