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<p>characterized by <a href="page.php?w=flood_basalt">flood basalt</a>s and may progress to the point where a tectonic plate is completely split. A divergent plate boundary then develops between the two-halves of the split plate. However, rifting often fails to completely split the continental lithosphere (such as in an <a href="page.php?w=aulacogen">aulacogen</a>), and failed rifts are characterized by volcanoes that erupt unusual <a href="page.php?w=Alkaline_magma_series">alkali lava</a> or <a href="page.php?w=carbonatite">carbonatite</a>s. Examples</p><p>
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