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Characterization and potential toxicity of asbestiform erionite from Gawler Downs, New Zealand
Evaluation of case-based reasoning to estimate liquefaction manifestation
Rapid Earthquake Rupture Characterization for New Zealand Using the FinDer Algorithm
Parametric Testing of EQTransformer’s Performance against a High‐Quality, Manually Picked Catalog for Reliable and Accurate Seismic Phase Picking
Fluvial geomorphic factors affecting liquefaction-induced lateral spreading
The influence of multiple impedance contrasts on mHVSR site period estimates in the Canterbury Plains of New Zealand and implications for site classification
The Estimated Carbon Cost of Concrete Building Demolitions following the Canterbury Earthquake Sequence
The Effect of Seismic Sequences in Probabilistic Seismic Hazard Analysis
The influence of off-fault deformation zones on the near-fault distribution of coseismic landslides
CPT-based liquefaction case histories compiled from three earthquakes in Canterbury, New Zealand
A near-real-time model for estimating probability of road obstruction due to earthquake-triggered landslides
An exploration of the use of machine learning to predict lateral spreading
Challenges in the definition of input motions for forensic ground-response analysis in the near-source region
Seismic performance of a retrofitted heritage unreinforced masonry building during the 2010/2011 Canterbury earthquakes
Highly localized upper mantle deformation during plate boundary initiation near the Alpine fault, New Zealand
Seismicity Rate Change as a Tool to Investigate Delayed and Remote Triggering of the 2010–2011 Canterbury Earthquake Sequence, New Zealand
A hidden Rodinian lithospheric keel beneath Zealandia, Earth's newly recognized continent
ABSTRACT An extensive kame-terrace sequence in the middle Rangitata Valley reveals ice-volume fluctuations spanning the last (Otiran) glaciation. Stratigraphic and sedimentologic characteristics document lateral ice-marginal processes and provide context for luminescence dating. The sequence provides novel and complementary data on glacier ice thickness, which fluctuated substantially throughout the Otiran glaciation. Thick ice constructed one of the highest kame terraces (540 m above the valley floor) ca. 68 ka and thinned nearly 500 m to the valley floor by ca. 53 ka. Following an episode of ice thickening to an unknown elevation, ice again thinned to the valley floor by ca. 44 ka. Ice thickened to its greatest late marine oxygen isotope stage (MIS) 3 extent of 480 m by ca. 37 ka, and thinned to 230 m by ca. 31 ka. The final ice expansion, to 260 m, occurred by ca. 25.5 ka, and the ice fluctuated and thinned to 240 m at ca. 22–20 ka and to 170 m at ca. 21–17 ka. Published cosmogenic radionuclide (CRN) ages indicate surface stabilization near the valley floor (55 m) by ca. 18 ka. This ice-thickness chronology provides an independently derived ice-volume record that is consistent with local and regional glacial chronologies. The site, lying between the Mackenzie Basin and the northern Canterbury Plains drainages, displays a chronology with advances correlative in part with each of those regions. Maximum ice extent occurred 70–65 ka in the Rangitata Valley and the Mackenzie Basin, while the subsequent ice expansion ca. 37 ka is similar in timing to chronologies in both the Rakaia Valley to the north and the Mackenzie Basin to the south.