<?xml version="1.0" encoding='utf-8'?>
<!DOCTYPE wml PUBLIC "-//WAPFORUM//DTD WML 1.1//EN" "http://www.wapforum.org/DTD/wml_1.1.xml">
<wml>
<card id="card1" title="Seismic magnitude scales - Page 5 - Wikipedia">
<p>
<a accesskey="1" href="page.php?w=Seismic_magnitude_scales&amp;p=4">1.Previous</a><br />
<a accesskey="3" href="page.php?w=Seismic_magnitude_scales&amp;p=6">3.Next</a>
</p>
<p>from the source, while sedimentary basins will often resonate, increasing the duration of shaking. This is why, in the <a href="page.php?w=1989_Loma_Prieta_earthquake">1989 Loma Prieta earthquake</a>, the <a href="page.php?w=Marina_District%2C_San_Francisco">Marina district of San Francisco</a> was one of the most damaged areas, though it was nearly 100&nbsp;km from the epicenter. Geological structures were also significant, such as where seismic waves passing under the south end of <a href="page.php?w=San_Francisco_Bay">San Francisco Bay</a> reflected</p><p>
<a accesskey="1" href="page.php?w=Seismic_magnitude_scales&amp;p=4">1.Previous</a><br />
<a accesskey="3" href="page.php?w=Seismic_magnitude_scales&amp;p=6">3.Next</a>
</p>

<do type="prev" label="Search">
        <go href="search.wml"/>
</do>

</card>
</wml>
