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The quake of 22 Feb 2011 was Richter 6.3, but was very close to a major town (10km) and quite shallow (<10km). Some of its aftershocks were as shallow as 1km!

Ground accelerations may have been as high as 2G at some frequencies.

It is very difficult to design structures for greater than 1G.

There are three important elements in how am earthquake affects a building; the sizer of the quake; the transmission path to a particular site, including that of the specific building site; and the design of the building itself.

Due to ground resonances, the Q (the degree of amplification of the seismic forces) of ordinary sites is around 3 to 5. For a rock site it will be close to 1. For a swampy area, it will head towards 10. Mexico City holds the palm (I believe) for the highest Q, which reaches 15 at some frequencies important to seismicity.

That means that the ground acceleration will commonly be several times that of the native acceleration at that site.

A further problem is that of unstable sites. If you have a look at the Niigata Earthquake photos, you'll see several perfectly sound multi storey accommodation buildings, except they are up to 30 deg from plumb!

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13y ago
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14y ago

In 1931 the Napier earthquake killed 255 people that was New Zealand's worst earthquake.

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Q: What Day was the big earthquake in New Zealand?
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