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Advances in Noninvasive Approaches to Characterizing Seismic Site Conditions
Conveners: Alan Yong, USGS, Sheri Molnar, University of Western Ontario, and Aysegul Askan, Middle East Technical University
Site effects associated with near-surface geological conditions constitute an important part of any seismic hazard assessment. In situ measurements of shear-wave velocity (VS) are commonly used to evaluate the seismic response of sites under investigation. Traditional invasive approaches “directly” measure VS; however, these methods are often costly and (or) environmentally prohibitive. In comparison, non-invasive methods (using body- and surface-waves) are generally more cost-effective and by nature, considered environmentally friendly. Thus, the appeal and use of non-invasive methods has significantly increased in recent years. Non-invasive methods, however, do not directly measure VS and have inherent uncertainties. The purpose of this session is to facilita
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THE NEW ZEALAND OFFICIAL YEAR-BOOK, 1960
EARLY HISTORY: General.—When New Zealand was discovered by Europeans in 1642 it was found to be inhabited by a race of Polynesians called Maoris, who had migrated to these islands many centuries previously. At what time the discovery of New Zealand was made by the Maoris, and from what country they came, cannot be stated accurately, for being an unlettered people they had only oral records of their history. The origins of the Maori people prior to their final migration are even more obscure, but in accordance with the general tradition of the Polynesian race it would seem that from Asia they migrated eastward by way of Malaysia to the Pacific. According to their mythology their Pacific home was the island of Hawaiki—the position of which is now unknown—and from t
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