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<p>in Libya, is located in the north of the range. The central third of the Tibesti is of volcanic origin and consists of five <a href="page.php?w=volcano">volcano</a>es topped by large depressions: Emi Koussi, <a href="page.php?w=Tarso_Toon">Tarso Toon</a>, <a href="page.php?w=Tarso_Voon">Tarso Voon</a>, <a href="page.php?w=Tarso_Yega">Tarso Yega</a> and <a href="page.php?w=Toussid%C3%A9">Toussidé</a>. Major <a href="page.php?w=lava_flow">lava flow</a>s have formed vast plateaus that overlie <a href="page.php?w=Paleozoic">Paleozoic</a> sandstone.</p><p>
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