<html><head><meta http-equiv="Content-Type" content="text/html charset=utf-8"></head><body style="word-wrap: break-word; -webkit-nbsp-mode: space; -webkit-line-break: after-white-space;" class=""><div class="">Dear all,</div><div class=""><br class=""></div><div class="">the Friday seminar series continues next Friday (5 May) at 12:30 in the seminar room on the 3rd floor with a presentation given by:</div><div class=""><br class=""></div><div class=""><br class=""></div><div class=""><div class=""><span class=""><span class="">John Haines: </span><span class=""><b class="">"The Darfield Mw 7.1 earthquake of 4 September 2010 and the Christchurch Mw 6.3 aftershock of 22 February 2011</b></span></span><b class="">”</b></div><div class=""><span class=""><br class=""></span></div><div class=""><span class="">The M7.1 Darfield main shock ruptured the Greendale fault in 2010, rupturing a previously unknown fault, now termed the Greendale fault. The Christchurch main shock also ruptured an unknown active fault. Both events caused significant damage and loss of lives. A large number of scientist has been studying these events since, and this talk summarises the main findings.</span></div><div class=""><div class=""><p class="MsoNormal"><span lang="EN-NZ" class="">These include:</span></p><p class="MsoNormal" style="margin-left: 36pt; text-indent: -18pt;"><span style="font-family: Arial;" class="">•<span style="font-size: 7pt; font-family: 'Times New Roman';" class=""> </span></span><span lang="EN-NZ" class="">Source models: from seismology and geodesy</span><o:p class=""></o:p></p><p class="MsoNormal" style="margin-left: 36pt; text-indent: -18pt;"><span style="font-family: Arial;" class="">•<span style="font-size: 7pt; font-family: 'Times New Roman';" class=""> </span></span><span lang="EN-NZ" class="">Hydrology: Canterbury Plains and elsewhere</span><o:p class=""></o:p></p><p class="MsoNormal" style="margin-left: 36pt; text-indent: -18pt;"><span style="font-family: Arial;" class="">•<span style="font-size: 7pt; font-family: 'Times New Roman';" class=""> </span></span><span lang="EN-NZ" class="">Kaiapoi: Liquifaction in Darfield EQ</span><o:p class=""></o:p></p><p class="MsoNormal" style="margin-left: 36pt; text-indent: -18pt;"><span style="font-family: Arial;" class="">•<span style="font-size: 7pt; font-family: 'Times New Roman';" class=""> </span></span><span lang="EN-NZ" class="">Port Hills: Rock fall and such in Christchurch EQ</span><o:p class=""></o:p></p><p class="MsoNormal" style="margin-left: 36pt; text-indent: -18pt;"><span style="font-family: Arial;" class="">•<span style="font-size: 7pt; font-family: 'Times New Roman';" class=""> </span></span><span lang="EN-NZ" class="">General damage: Both earthquakes and where to rebuild</span><o:p class=""></o:p></p><p class="MsoNormal" style="margin-left: 36pt; text-indent: -18pt;"><span style="font-family: Arial;" class="">•<span style="font-size: 7pt; font-family: 'Times New Roman';" class=""> </span></span><span lang="EN-NZ" class="">Seismic waves: Site effect recording</span><o:p class=""></o:p></p><p class="MsoNormal" style="margin-left: 36pt; text-indent: -18pt;"><span style="font-family: Arial;" class="">•<span style="font-size: 7pt; font-family: 'Times New Roman';" class=""> </span></span><span lang="EN-NZ" class="">Extreme motions </span></p></div><span class=""><br class=""></span></div><div class=""><span class=""><br class=""></span></div><div class=""><span class=""><br class=""></span></div><span class="">Maren & Maria</span></div><div class=""><br class=""></div><br class=""><div class="">
<div style="color: rgb(0, 0, 0); letter-spacing: normal; orphans: auto; text-align: start; text-indent: 0px; text-transform: none; white-space: normal; widows: auto; word-spacing: 0px; -webkit-text-stroke-width: 0px; word-wrap: break-word; -webkit-nbsp-mode: space; -webkit-line-break: after-white-space;" class=""><div style="color: rgb(0, 0, 0); letter-spacing: normal; orphans: auto; text-align: start; text-indent: 0px; text-transform: none; white-space: normal; widows: auto; word-spacing: 0px; -webkit-text-stroke-width: 0px; word-wrap: break-word; -webkit-nbsp-mode: space; -webkit-line-break: after-white-space;" class=""><div style="color: rgb(0, 0, 0); letter-spacing: normal; orphans: auto; text-align: start; text-indent: 0px; text-transform: none; white-space: normal; widows: auto; word-spacing: 0px; -webkit-text-stroke-width: 0px; word-wrap: break-word; -webkit-nbsp-mode: space; -webkit-line-break: after-white-space;" class="">_____________________________</div><div style="color: rgb(0, 0, 0); letter-spacing: normal; orphans: auto; text-align: start; text-indent: 0px; text-transform: none; white-space: normal; widows: auto; word-spacing: 0px; -webkit-text-stroke-width: 0px; word-wrap: break-word; -webkit-nbsp-mode: space; -webkit-line-break: after-white-space;" class="">Maria H. Janebo<br class="">Postdoctoral Research Fellow<br class=""><br class="">Nordic Volcanological Center<br class="">Institute of Earth Sciences<br class="">University of Iceland, Askja 223<br class="">Sturlugata 7, 101 Reykjavik, Iceland</div></div></div>
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