The decision on what to do with Christchurch's earthquake damaged redzone is one step closer, with the end of the public consultation period on the plan for the area. Over the past month Christchurch people have been asked to comment on a draft land use plan for the 602 hectares of land. Now those pitching ideas want the authorities to get on with the next step, so they can have some certainty about whether their projects can go ahead.
Fleur Beale is one of New Zealand's most prolific authors and the winner of many awards for children and young adult books. Her latest work is a novel that tells the story of a young girl who experienced the February 2011 Christchurch earthquake. It's part of an international series called Through my Eyes - Natural Disaster Zones, which is a series written by different authors focusing on war zones and disasters throughout the world. Fleur's book is based on real accounts of what happened in Christchurch told through the eyes of a young girl, Lyla. Fleur, who has won the Margaret Mahy Medal for her outstanding contribution to children's writing, and was awarded the New Zealand Order of Merit for services to literature, joins Kathryn to talk about her latest work, and why young adult fiction is the best and the process of getting a story right.
The Canterbury earthquakes have provided the opportunity to reconsider the Christchurch CBD - and arts and culture have often led the discussion. No more so than during the bold biennial weekend celebration of urban creativity which is Festa, which first gave the public access to the red zone back in in 2012. FESTA returns this Labour weekend and joining Mark Amery this week are festival director and architectural historian Doctor Jessica Halliday and Kairaranga or weaver Benita Wakefield, who is part of FESTA project Kono for Kai.
The Leader Fault was one of at least 17 faults that ruptured the ground surface across the northeastern South Island of New Zealand during the Mw 7.8 2016 Kaikōura Earthquake. The southern ~6 km of the Leader Fault, here referred to as the South Leader Fault (SLF), ruptured the North Canterbury (tectonic) Domain and is the primary focus of this study. The main objective of the thesis is to understand the key factors that contributed to the geometry and kinematics of the 2016 SLF rupture and its intersection with The Humps Fault (HF). This thesis employs a combination of techniques to achieve the primary objective, including detailed mapping of the bedrock geology, geomorphology and 2016 rupture, measurement of 2016 ground surface displacements, kinematic analysis of slip vectors from the earthquake, and logging of a single natural exposure across a 2016 rupture that was treated as a paleoseismic trench. The resulting datasets were collected in the field, from terrestrial LiDAR and InSAR imagery, and from historical (pre-earthquake) aerial photographs for a ~11 km2 study area. Surface ruptures in the study area are a miniature version of the entire rupture from the earthquake; they are geometrically and kinematically complex, with many individual and discontinuous segments of varying orientations and slip senses which are distributed across a zone up to ~3.5 km wide. Despite this variability, three main groups of ruptures have been identified. These are: 1) NE-SW striking, shallow to moderate dipping (25-45°W) faults that are approximately parallel to Cenozoic bedding with mainly reverse dip-slip and, and for the purposes of this thesis, are considered to be part of the SLF. 2) N-S striking, steeply dipping (~85°E) oblique sinistral faults that are up to the west and part of the SLF. 3) E-NE striking, moderate to steeply dipping (45-68°N) dextral reverse faults which are part of the HF. Bedding-parallel faults are interpreted to be flexural slip structures formed during folding of the near-surface Cenozoic strata, while the steeply dipping SLF ruptured a pre-existing bedrock fault which has little topographic expression. Groups 1 and 2 faults were both locally used for gravitational failure during the earthquake. Despite this non-tectonic fault movement, the slip vectors for faults that ruptured during the earthquake are broadly consistent with NCD tectonics and the regional ~100-120° trend of the principal horizontal stress/strain axes. Previous earthquake activity on the SLF is required by its displacement of Cenozoic formations but Late Quaternary slip on the fault prior to 2016 is neither supported by pre-existing fault scarps nor by changes in topography across the fault. By contrast, at least two earthquakes (including 2016) appear to have ruptured the HF from the mid Holocene, consistent with recurrence intervals of no more than ~7 kyr, and with preliminary observations from trenches on the fault farther to the west. The disparity in paleoearthquake records of the two faults suggests that they typically do not rupture together, thus it is concluded that the HF-SLF rupture pattern observed in the Kaikōura Earthquake rarely occurs in a single earthquake.
