Just after half four on the morning of September 4th, a M7.0 earthquake epicentered 40km west of Christchurch, thoroughly shaking the region and causing an estimated $2 billion in damages. East Christchurch was hit especially hard due to ground liquefaction and an abundance of brick buildings. Miraculously no one was killed and I only heard reports of two people being injured. Some impressive images of the damage can be found on the web.This earthquake caught all geologists off-guard as there was zero evidence for active faulting in the area and Christchurch was thought to have a relatively low seismic hazard compared to the rest of the South Island. This earthquake changes everything and throws a wrench in established models of seismic hazard in NZ. It's a good time to be a pessimistic geologist!
I was passing through the general area on the morning of the 11th with my parents so we decided to take a detour to see the surface rupture along the country roads. By this time all of the roads were unfortunately repaired such that the cracks were no longer present in the road. For about 20km, formerly straight roads now have a noticeable kink to the right when you cross the fault. Large stands of trees in forestry blocks were mostly intact apart from trees within about 30m of the fault trace, which had either been uprooted or, in some cases, snapped on their trunks. Visible damage to nearby structures was minor apart from a few brick walls and buildings. Focal mechanisms and surface ruptures both show dextral strike-slip (horizontal) offset (of up to 4m) with a slight reverse (vertical) component on a steep-dipping fault plane. Good images can be found on GNS Science's website.
Above: En echelon tension gashes rupture a ~15m wide zone in a paddock along the fault rupture.
Dextral road offset of a whole lane (~3m)















































