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<p>as <a href="page.php?w=seamount">seamount</a>s and later as fully-fledged <a href="page.php?w=volcanic_islands">volcanic islands</a>. The local <a href="page.php?w=tectonic_plate">tectonic plate</a> (in the case of the Hawaii hotspot, the <a href="page.php?w=Pacific_Plate">Pacific Plate</a>) gradually passes over the hotspot, carrying its volcanoes with it without affecting the plume. Over hundreds of thousands of years, the magma supply for an individual volcano is slowly cut off, eventually causing its extinction. No longer active enough to</p><p>
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