<?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="Fissure vent - Page 5 - Wikipedia">
<p>
<a accesskey="1" href="page.php?w=Fissure_vent&amp;p=4">1.Previous</a><br />
<a accesskey="3" href="page.php?w=Fissure_vent&amp;p=6">3.Next</a>
</p>
<p>fissures. This distribution of vents and sometimes voluminous eruptions of fluid basaltic lava usually builds up a thick lava plateau, rather than a single volcanic edifice. But there are also the <a href="page.php?w=central_volcano">central volcano</a>es, <a href="page.php?w=composite_volcano">composite volcano</a>es, often with <a href="page.php?w=caldera">caldera</a>s, which have been formed during thousands of years, and eruptions with one or more magma reservoirs underneath controlling their respective fissure system.</p>

<p>The <a href="page.php?w=Laki">Laki</a></p><p>
<a accesskey="1" href="page.php?w=Fissure_vent&amp;p=4">1.Previous</a><br />
<a accesskey="3" href="page.php?w=Fissure_vent&amp;p=6">3.Next</a>
</p>

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

</card>
</wml>
