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are important. Investigations addressing the dynamic geomorphic                              identified in Canterbury buildings and observed versus predicted              GSA TODAY | www.geosociety.org/gsatoday/
responses of urban rivers and coastal plains to relative sea-level                           performance: Earthquake Spectra, v. 30, p. 335–362, doi: 10.1193/
rise, shoreline retreat, groundwater responses, liquefaction,                                021513EQS028M.
subsidence, and coastal aquifer resources are all urgently required.                   Bradley, B.A., 2012, Strong ground motion characteristics observed in the
In parallel with these scientific considerations, there also needs to                        4 September 2010 Darfield, New Zealand earthquake: Soil Dynamics and
be a focus on how current policies, planning, and socio-economic                             Earthquake Engineering, v. 42, p. 32–46, doi: 10.1016/j.soildyn.2012.06.004.
contexts will influence trajectories of urban form, and to what                        Bradley, B.A., and Cubrinovski, M., 2011, Near-source strong ground motions
degree these will influence the exposure of current and future                               observed in the 22 February 2011 Christchurch Earthquake: Seismological
communities to continued flooding and sea-level rise.                                        Research Letters, v. 82, no. 6, p. 853–865, doi: 10.1785/gssrl.82.6.853.
                                                                                       Bradley, B.A., Quigley, M.C., Van Dissen, R.J., and Litchfield, N.J., 2014, Ground
  The anthropogenic intervention of long-term geologic processes                             motion and seismic source aspects of the Canterbury Earthquake Sequence:
that previously enabled sediment aggradation to rebuild topog-                               Earthquake Spectra, v. 30, p. 1–15, doi: 10.1193/030113EQS060M.
raphy in this area means that subsidence will continue to domi-                        Briggs, R.W., Sieh, K., Meltzner, A.J., Natawidjaja, D., Galetzka, J., Suwargadi,
nate the topographic evolution of Christchurch. Similar scenarios,                           B., Hsu, Y.-J., Simons, M., Hananto, N., Suprihanto, I., Prayudi, D.,
where prograding sediment has been diverted from subsiding                                   Avouac, J.-P., Prawirodirdjo, L., and Bock, Y., 2006, Deformation and slip
areas, are likely to plague coastal settlements worldwide. Strong                            along the Sunda megathrust in the great 2005 Nias-Simeulue earthquake:
earthquakes sourced from previously unidentified and/or blind                                Science, v. 311, p. 1897–1901, doi: 10.1126/science.1122602.
faults and their impacts on flood and relative sea levels add to the                   Brock, J.C., and Purkis, S.J., 2009, The emerging role of LiDAR remote sensing
myriad of short- to long-term challenges facing coastal environ-                             in coastal research and resource management: Journal of Coastal
ments throughout the world.                                                                  Research, Special Issue 53, p. 1–5, doi: 10.2112/SI53-001.1.
                                                                                       Brown, L.J., and Weeber, J.H., 1992, Geology of the Christchurch Urban Area:
  Future investigations of the impacts of relative sea-level rise on                         GNS Science, scale 1:25:000, 104 p.
coastal populations should consider the role of earthquakes,                           Canterbury Regional Council, 1993, Avon and Heathcote catchment, rivers and
including those that may be sourced from unknown and/or prox-                                estuary: Issues and options for managing the Heathcote River floodplain:
imal faults, in reshaping coastal topography and thus influencing                            Canterbury Regional Council Report R93(1), 43 p.
the dynamics of coastal and flood hazards. As shown here, this is                      Canterbury Regional Council, 1997, Avon River: Issues and options for
particularly important for densely populated, low-lying, and                                 managing the Avon River floodplain: Canterbury Regional Council
tectonically active regions built upon youthful and liquefiable                              Report R97(1), 41 p.
alluvial and marine sediments.                                                         Cazenave, A., Dieng, H., Meyssignac, B., Von Schuckmann, K., Decharme, B.,
                                                                                             and Berthier, E., 2014, The rate of sea-level rise: Nature Climate Change,
ACKNOWLEDGMENTS                                                                              v. 4, p. 358–361, doi: 10.1038/nclimate2159.
                                                                                       CCC, 2014, Flood extent models, Christchurch city council flood modeling
   We thank the New Zealand Earthquake Commission for research                               data, hosted by the Canterbury Earthquake Recovery Authority: http://
capability funding and for provision of LiDAR data. These and other                          maps.cera.govt.nz/advanced-viewer/?Viewer=Ccc-Floor-Levels (last
                                                                                             accessed 12 Dec. 2014).
   data are available on the Canterbury Geotechnical Database (https://                Center for Advanced Engineering, 1995, Risks and Realities—A Multidisciplinary
canterburygeotechnicaldatabase.projectorbit.com/). We also thank                             Approach to the Vulnerability of Lifelines to Natural Hazards: Report of
Environment Canterbury and the New Zealand Ministry of Business,                             the Christchurch Engineering Lifelines Group: Christchurch, New
Innovation and Employment (MBIE contract UOCX0902) for funding                               Zealand, University of Canterbury, Center for Advanced Engineering, 312 p.
analyses of the Avon-Heathcote Estuary.                                                Cox, S.C., Rutter, H.K., Sims, A., Manga, M., Weir, J.J., Ezzy, T., White, P.A.,
                                                                                             Horton, T.W., and Scott, D., 2012, Hydrological effects of the MW 7.1
REFERENCES CITED                                                                             Darfield (Canterbury) earthquake, 4 September 2010: New Zealand
                                                                                             Journal of Geology and Geophysics, v. 55, no. 3, p. 231–247, doi: 10.1080/
Aerts, J.C.J.H., Botzen, W.J.W., Emanuel, K., Lin, N., and De Moel, H., 2014,                00288306.2012.680474.
      Evaluating flood resilience strategies for coastal megacities: Science, v. 344,  Cubrinovski, M., Hughes, M., Bradley, B., Noonan, J., Hopkins, R., McNeill, S.,
      p. 473–475, doi: 10.1126/science.1248222.                                              and English, G., 2014a, Performance of horizontal infrastructure in
                                                                                             Christchurch City through the 2010–2011 Canterbury Earthquake
Basher, L.R., Hicks, D.M., McSaveny, M.J., and Whitehouse, I.E., 1988, The                   Sequence: University of Canterbury, Civil & Natural Resources
      lower Waimakariri River floodplain: A geomorphological perspective:                    Engineering Research Report 2014-02, March 2014, 129 p.
      A report for North Canterbury Catchment Board, 33 p.                             Cubrinovski, M., Hughes, M., and O’Rourke, T., 2014b, Impacts of liquefaction
                                                                                             on the potable water system of Christchurch in the 2010–2011 Canterbury
Beavan, J., Samsonov, S., Motagh, M., Wallace, L., Ellis, S., and Palmer, N.,                (NZ) earthquakes: Journal of Water Supply: Research & Technology–Aqua,
      2010, The Darfield (Canterbury) Earthquake: Geodetic observations and                  v. 63, p. 95–105, doi: 10.2166/aqua.2013.004.
      preliminary source model: Bulletin of the New Zealand Society for                Cubrinovski, M., Winkley, A., Haskell, J., Palermo, A., Wotherspoon, L.,
      Earthquake Engineering, v. 43, p. 228–235.                                             Robinson, K., Bradley, B., Brabhaharan, P., and Hughes, M., 2014c,
                                                                                             Spreading-induced damage to short-span bridges in Christchurch:
Beavan, J., Fielding, E., Motagh, M., Samsonov, S., and Donnelly, N., 2011,                  Earthquake Spectra, v. 30, p. 57–83, doi: http://dx.doi.org/10.1193/
      Fault location and slip distribution of the 22 February 2011 MW 6.2                    030513EQS063M.
      Christchurch, New Zealand, Earthquake from geodetic data: Seismological          Dixon, T.H., Amelung, F., Feretti, A., Novali, F., Rocca, F., Dokka, R., Sella,
      Research Letters, v. 82, p. 789–799, doi: 10.1785/gssrl.82.6.789.                      G., Kim, S.-W., Wdowinski, S., and Whitman, D., 2006, Subsidence and
                                                                                             flooding in New Orleans: Nature, v. 441, p. 587–588, doi: 10.1038/
Beavan, J., Levick, S., Lee, J., and Jones, K., 2012a, Ground displacements and dila-        441587a.
      tional strains caused by the 2010–2011 Canterbury earthquakes: GNS Science       Downes, G., and Yetton, M., 2012, Pre-2010 historical seismicity near
      Consultancy Report 2012/67.59, https://canterburygeotechnicaldatabase                  Christchurch, New Zealand: The 1869 MW 4.7–4.9 Christchurch and 1870
      .projectorbit.com (last accessed 12 Dec. 2014).                                        MW 5.6–5.8 Lake Ellesmere earthquakes: New Zealand Journal of Geology
                                                                                             and Geophysics, v. 55, no. 3, p. 199–205, doi: 10.1080/00288306
Beavan, J., Motagh, M., Fielding, E.J., Donnelly, N., and Collett, D., 2012b, Fault          .2012.690767.
      slip models of the 2010–2011 Canterbury, New Zealand, earthquakes from
      geodetic data and observations of postseismic ground deformation: New
      Zealand Journal of Geology and Geophysics, p. 37–41, doi: 10.1080/
      00288306.2012.697472.

Bech, D., Cordova, P., Tremayne, B., Tam, K., Weaver, B., Wetzel, N., Parker,
      W., Oliver, L., and Fisher, J., 2014, Common structural deficiencies

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