“…The CES initiated with the M w 7.1, 4 September 2010 Darfield earthquake and was punctuated by the M w 6.2, 22 February 2011 Christchurch earthquake, each of which induced pervasive and damaging liquefaction. Observed manifestations of liquefaction included, among others: (1) spreading-and settlement-induced damage to bridges and bridge approaches (e.g., [58,20]); (2) widespread loss of road functionality due to cracking and fissuring of pavements and inundation by liquefaction ejecta (e.g., [17]); (3) failure of buried lifelines due to flotation or differential settlements, to include water and wastewater distribution systems (e.g., [44]), electric power networks (e.g., [34]), and communication lines (e.g., [53]); (4) damage to levees (stopbanks) caused by spreading, Contents lists available at ScienceDirect journal homepage: www.elsevier.com/locate/soildyn slumping, and settlement (e.g., [23]); (4) impairment of port structures caused by ground deformations, to include wharfs, seawalls, and fuel lines (e.g., [13]); (5) slumping-and spreadinduced damage to railway embankments (e.g., [17]); and (7) settlement and tilting of residential homes, commercial properties, and high-rise structures, resulting in widespread loss of building stock (e.g., [9]). In addition to direct effects on infrastructure, the $500,000 t of liquefaction ejecta collected throughout Christchurch posed a threat to stormwater systems and to human health if left unmanaged [57].…”