Seddon

Liquefaction Effects from the Cook Strait / Lake Grassmere Quakes

The recent magnitude 6.5 Cook Strait and  6.6 Lake Grassmere earthquakes were comparable in size to the ‘quakes that rattled Canterbury in 2010 and 2011.  This map of peak ground accelerations for the Lake Grassmere Earthquake shows recordings of up to about 0.75g.(or 0.75  the acceleration due to gravity). One of the notorious and extremely damaging effects of groundshaking in Christchurch was the widespread liquefaction and flooding that affected large areas in the eastern suburbs. This occurred in areas where the land was made up of soft low lying sediments by the river or near the coast such as Bexley and Avonside. (photo by Dick Beetham, GNS Science)The most significant damage in Wellington was long the edge of the port where a large section of the road collapsed into the sea. This photo by Graham Hancox of GNS Science, shows the scene after the combined effects of the two recent earthquakes. So what were the effects on the ground near the earthquake epicentres? Are there any areas of soft, waterlogged sediments beside an estuary or river in Marlborough that might be expected to compare with those severely damaged parts of Christchurch? A team from GNS Science went to look at the ground damage alongside the Opawa River, near its confluence with the Wairau River. Dougal Townsend took these photos during their visit: Near to the river, there were several long cracks created by lateral spreading. Sand boils and sand volcanoes had left their mark over the paddocks beside the river. With the help of a spade, one of the sand volcanoes was sliced vertically to show a clean cross section through it. You can see the thin crack in the soil that was opened up during the earthquake, that allowed the sand loaded water to ‘erupt’ at the surface. Compared to Christchurch, these liquefaction effects from the recent Cook Strait and Lake Grassmere Earthquakes are relatively minor. This is an important finding as it shows that the extreme level of liquefaction in Christchurch was not necessarily a typical example of what to expect from future earthquakes in the rest of the country. Scientists now have some more useful data to help to differentiate between the impacts of ‘quakes in apparently similar environments.

Liquefaction Effects from the Cook Strait / Lake Grassmere Quakes Read More »

Lake Grassmere Quakes

Following the earthquakes in southern cook straight, the GeoNet rapid response team left immediately to place seismometers around the area, to allow more detailed monitoring and get better information with which to model the fault ruptures. This meant that when the Mag 6.6 occurred, the enhanced array of seismometers was already in place. Here is a screen shot of the Mag 6.6 Grassmere Earthquake and immediate aftershocks over the following hours: This GeoNet video gives an idea of the number and locations of aftershocks from the 16th to19th August

Lake Grassmere Quakes Read More »

Earthquakes in Southern Cook Strait

This is a screen shot of the Wellington seismometer from very early on Monday morning 22 July Following the earthquakes in Cook Strait over the weekend, it was impressive to arrive at work on Monday morning, and watch how the GeoNet team, many of whom had been busy right through the weekend, were in full action mode again. Ken Gledhill, the head of GeoNet, co-ordinated two meetings of the scientists and technicians during the day. There are lots of different things involved with understanding earthquakes. These include getting accurate locations and magnitudes, modelling the position and orientation of the fault and the type of fault rupture from the seismic wave patterns of the aftershocks, working out the adjusted stress on nearby active faults and then trying to calculate probabilities of future quakes to inform an ‘awakened’ public… Here is the aftershock map from Sunday evening that shows the relative magnitudes of the quakes and their initial locations in 2 dimensions. Up to today there have been nearly one thousand aftershocks already. As more and more occur and get analysed, a more precise 3D image of the fault(s) involved will be built up. To help get more precise seismic data, the GeoNet fast response team are already in Marlborough, setting up some extra temporary seismometers at carefully chosen locations to ‘fill in the gaps’ between existing permanent stations. Here is a photo of one of the team yesterday, packing one of the seismometers for the trip. To see more photos of what these guys do, have a look here. This is a computer simulation of the seismic waves from the M6.5 ‘quake propagating across the North Island and the adjacent sea floor: New Zealand’s background risk of earthquake probabilities has been calculated for the whole country. Once a reasonably large earthquake has occurred, these background risks of a larger quake increase for a while in the local area, and  a sequence of aftershocks follows that typically fits into a fairly predictable pattern of decreasing intensity over time. In the video below Matt Gerstenberger explains how these calculations are made to produce probability tables and maps for future aftershocks. For the latest information about the number and magnitude of aftershocks that have occurred in Cook Strait, as well as forecast probabilities for future quakes, have a look at this GeoNet page

Earthquakes in Southern Cook Strait Read More »