Landslides and Landslide dams caused by the Kaikoura Earthquake. New Zealand media reported that a 100-year-old woman and her daughter-in-law were pulled out alive from their home in Kaikoura, after the house collapsed in the first earthquake. That’s a good thing, we aren’t complaining. The New Zealand Earthquake Commission had received around 38,000 residential claims for damage caused by March 2017. The Kaikoura Mw7.8 earthquake struck at 12.03 am local time on 14th November 2016 (UTC: 11.03 am 13th November 2016) – a shallow (15 km) magnitude 7.8 earthquake (Mw), with an epicentre located near Waiau in North Canterbury (Kaiser et al, 2017), and strongly shook the North Canterbury and Marlborough regions of NZ.

Just after midnight on 14 November 2016, a 7.8 magnitude earthquake struck New Zealand’s South Island, roughly 60km south-west of the coastal town of Kaikoura. Starting in Culverdon, 70km south of Kaikōura, the quake ripped across several fault lines, including one that was previously unknown. by the 14 November 2016 Kaikoura earthquake, South Island, New Zealand 2 North Canterbury and Marlborough regions of NZ. Huge slips, caused by the 7.5 magnitude earthquake, are seen blocking State Highway One north of Kaikoura. The Kaikoura earthquake caused extremely complex surface ruptures to form on at least 9 different faults. The Kaikoura quake produced the strongest ground shaking ever recorded for an earthquake in New Zealand, a new study has found. While repair work is underway, the long-term significance of …

The strong ground shaking caused damage to buildings and infrastructure across the northeast of the South Island. Information for surveyors about the 2016 Kaikoura earthquakes. Ground movements. On Monday 14 November 2016, the magnitude 7.8 Kaikoura Earthquake resulted in ground movements exceeding 5cm from the middle of the South Island to the bottom of the North Island.

The moment the Kaikoura earthquake struck. A consequence … The majority of claims lodged are for building damage only (71%), 10% for building and contents, 9% contents only and 10% land damage. Looking around Kaikoura … The Kaikoura earthquake struck just after midnight on November 14, devastating Kaikoura and causing major problems in Wellington. Photograph: Pool/Getty Images A small town at … One hazard we don’t often get an opportunity to talk about at GeoNet is landslides.

Seismic energy was released for nearly 2 minutes. The 2016 Kaikoura earthquake was a magnitude 7.8 (M w) earthquake in the South Island of New Zealand that occurred two minutes after midnight on 14 November 2016 NZDT (11:02 on 13 November UTC). The ruptures travelled 170 km along the South Island’s north-east coast. The largest wave was 6.9m in the Goose Bay area, just south of Kaikōura.

The earthquake rupture (movement on the faults) propagated south-west to north-east through the North Canterbury and Marlborough Fault areas- essentially "unzipping" along an approximately 180km length of the northeast coast of the South Island (Watching the M7.8 Kaikoura Quake Dominos Fall in Real Time).The rupture lasted nearly 2 minutes in total, and where the faults … Serious damage to road and rail infrastructure was also experienced … (Photo courtesy of Dr. Kate Pedley, University of Canterbury) Several massive landslide dams were caused by the Kaikoura earthquake. The initial rupture started on a fault near Culverden and then jumped from fault to fault as it moved at a speed of 2 km/s. Ruptures occurred on multiple faults and the earthquake has been described as the "most complex earthquake ever studied". This image was taken to the north of the fault scarp shown in the first image. The earthquake caused two fatalities: one man was killed in the collapse of the Kaikoura Elms Homestead; one woman died following the impact of the event on the Mount Lyford log cabin where she lived. The Kaikoura Earthquake has caused significant disruption to families, infrastructure, and regional economies. The Kaikoura quake produced the strongest ground shaking ever recorded for an earthquake in New Zealand, a new study has found. The 2016 Mw 7.8 Kaikōura earthquake was a complex sequence of ruptures that included 12 major faults and nine lesser faults. Now, as reported by the New Zealand Herald, scientists have managed to photograph some of the fresh fractures that were caused by this incredibly powerful earthquake.

Several other areas had 3 to 4m waves. Kaikoura earthquake caused 'largest and most widespread episode of slow slip' seen in NZ • Source: 1 NEWS.

The strong ground shaking caused damage to buildings … In scientific terms, the Kaikōura earthquake was a new phenomenon.