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Cats, dogs, horses, parrots, rats, hedgehogs and turtles. Just like people, these animals were affected by the earthquakes in Christchurch. And two researchers have published a new book into just how big the impact of the September 2010 and February 2011 earthquakes were. 'Animals in Emergencies: Learning from the Christchurch Earthquakes' is co-authored by Canterbury University's associate professor Annie Potts, and former veterinary nurse Donelle Gadenne.
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The Earthquake Recovery Minister says Christchurch City Council must take responsibility for the city's flooding problems as it's not the government's problem to sort out.
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Three years on from the earthquakes of 2011, Census data now confirms massive changes to the face and shape of Christchurch.
A Christchurch resthome under stress after the earthquakes is being blamed for systemic failures that ended in a frail elderly woman dying.
In Christchurch today the Duke and Duchess of Cambridge took time to talk to some of the families of those who died in the February 2011 earthquake.
Active faults capable of generating highly damaging earthquakes may not cause surface rupture (i.e., blind faults) or cause surface ruptures that evade detection due to subsequent burial or erosion by surface processes. Fault populations and earthquake frequency-‐magnitude distributions adhere to power laws, implying that faults too small to cause surface rupture but large enough to cause localized strong ground shaking densely populate continental crust. The rupture of blind, previously undetected faults beneath Christchurch, New Zealand in a suite of earthquakes in 2010 and 2011, including the fatal 22 February 2011 moment magnitude (Mw) 6.2 Christchurch earthquake and other large aftershocks, caused a variety of environmental impacts, including major rockfall, severe liquefaction, and differential surface uplift and subsidence. All of these effects occurred where geologic evidence for penultimate effects of the same nature existed. To what extent could the geologic record have been used to infer the presence of proximal, blind and / or unidentified faults near Christchurch? In this instance, we argue that phenomena induced by high intensity shaking, such as rock fragmentation and rockfall, revealed the presence of proximal active faults in the Christchurch area prior to the recent earthquake sequence. Development of robust earthquake shaking proxy datasets should become a higher scientific priority, particularly in populated regions.
People often ask what we’re learning as a result of all this post-earthquake archaeology. Quite a lot, as this blog reveals. But, to date, the blog has focused on the individual sites and/or stories – there’s not been much of … Continue reading →
New research shows many Cantabrians are still struggling to cope with the after effects of the earthquakes.
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