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South Island of NZ is mostly F-E162 which makes sense as its the Pacific Plate side, but the lower part (of the South Island) is F-E161 which catches the southern part of Fiordland and the Puysegur Trench and Bank on the Australian Plate which is siesmically different,
and on the Australia Map you have the coast of NSW and Victoria as a seperate region to South Australia coast which do feature as independant siesmic areas when you check the GeoAu web site
This region is another example of how Flinn and Engdahl (1965) failed to accurately define a known tectonic feature. The feature is the West Chile Rise partly defined by Region 686, West Chile Rise, but some of the seismicity occurs to the south in Region 692, Southern Pacific Ocean. The region is in two parts and removes the earthquakes associated with the tectonic activity from region 692 which remains classed as aseismic. The seismic region remains as 43. Fig. 10 illustrates the reason for this region.
That pdf converted into a KML file useable on Google Earth would be handy I wonder if anyone is working on it
Originally posted by detachedindividual
Being a Sociology and Psychology geek, the responses of the population is something that interests me.
It would be interesting to see how the population number has changed over the last year, and see how that progresses.
We could see Christchurch become a ghost town over the next five to ten years.
We could see Christchurch become a ghost town over the next five to ten years.
1934-07-18T19:40:23.950Z -11.90700 166.73100 7.8000 Mw 35.0000
1934-07-21T06:18:23.290Z -11.13900 165.50300 7.1000 Mw 35.0000