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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
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