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<p>(0.001 Pa·s). Because of this very high viscosity, felsic lavas usually erupt explosively to produce <a href="page.php?w=Pyroclastic_rock">pyroclastic</a> (fragmental) deposits. However, rhyolite lavas occasionally erupt effusively to form <a href="page.php?w=lava_spine">lava spine</a>s, <a href="page.php?w=lava_dome">lava dome</a>s or "coulees" (which are thick, short lava flows).  The lavas typically fragment as they extrude, producing block lava flows. These often contain <a href="page.php?w=obsidian">obsidian</a>.</p>

<p>Felsic magmas can</p><p>
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