The historic Townsend Teece telescope in Otautahi Christchurch was badly damaged in the 2011 earthquake, but has been expertly restored and is now reinstalled back in its central city home at the Arts Centre.
A local developer is looking to reshape Ashburton's triangle, the historic retail centre of the town. Robert Grice owns a number of buildings on Victoria Street that require earthquake strengthening and he wants to redevelop the existing shops into a new mixed use hospitality precinct named The Ash. Jonathan also discusses an attempt to add quarter of a million dollars to ECan's annual plan budget which has been labelled a "slap in the face" by Environment Canterbury councillor Ian Mackenzie. And a hold-up of plumbing parts and red tape at the border means the Staveley Ice Rink won't be open to skaters and curlers until at least mid-June. Local Democracy Reporter - Mid Canterbury c from the Ashburton Guardian
We examined the stratigraphy of alluvial fans formed at the steep range front of the Southern Alps at Te Taho, on the north bank of the Whataroa River in central West Coast, South Island, New Zealand. The range front coincides with the Alpine Fault, an Australian-Pacific plate boundary fault, which produces regular earthquakes. Our study of range front fans revealed aggradation at 100- to 300-year intervals. Radiocarbon ages and soil residence times (SRTs) estimated by a quantitative profile development index allowed us to elucidate the characteristics of four episodes of aggradation since 1000 CE. We postulate a repeating mode of fan behaviour (fan response cycle [FRC]) linked to earthquake cycles via earthquake-triggered landslides. FRCs are characterised by short response time (aggradation followed by incision) and a long phase when channels are entrenched and fan surfaces are stable (persistence time). Currently, the Te Taho and Whataroa River fans are in the latter phase. The four episodes of fan building we determined from an OxCal sequence model correlate to Alpine Fault earthquakes (or other subsidiary events) and support prior landscape evolution studies indicating ≥M7.5 earthquakes as the main driver of episodic sedimentation. Our findings are consistent with other historic non-earthquake events on the West Coast but indicate faster responses than other earthquake sites in New Zealand and elsewhere where rainfall and stream gradients (the basis for stream power) are lower. Judging from the thickness of fan deposits and the short response times, we conclude that pastoral farming (current land-use) on the fans and probably across much of the Whataroa River fan would be impossible for several decades after a major earthquake. The sustainability of regional tourism and agriculture is at risk, more so because of the vulnerability of the single through road in the region (State Highway 6).