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<p>of lava domes can vary from <a href="page.php?w=basalt">basalt</a> (e.g. <a href="page.php?w=Semeru">Semeru</a>, 1946) to <a href="page.php?w=rhyolite">rhyolite</a> (e.g. <a href="page.php?w=Chait%C3%A9n_%28volcano%29">Chaiten</a>, 2010) although the majority are of intermediate composition (such as <a href="page.php?w=Santa_Mar%C3%ADa_%28volcano%29">Santiaguito</a>, <a href="page.php?w=dacite">dacite</a>-<a href="page.php?w=andesite">andesite</a>, present day). The characteristic dome shape is attributed to high viscosity that prevents the lava</p><p>
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