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<p><a href="page.php?w=explosive_eruption">explosive</a>, with compositions from <a href="page.php?w=basalt">basalt</a> to <a href="page.php?w=rhyolite">rhyolite</a>. Morphologically, centers include <a href="page.php?w=caldera">caldera</a>s, <a href="page.php?w=cinder_cone">cinder cone</a>s, <a href="page.php?w=stratovolcano">stratovolcano</a>es and small isolated <a href="page.php?w=lava">lava</a> masses. Due to repeated continental and alpine glaciations, many of the volcanic deposits in the belt reflect complex interactions between <a href="page.php?w=magma">magma</a></p><p>
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