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		<title>Calcaires roses br&#232;chiques du Danien</title>
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&lt;p&gt;Les br&#232;ches sont les t&#233;moins d'une instabilit&#233; (d&#233;formation syns&#233;dimentaire li&#233;e aux premiers mouvements tectoniques en rapport avec la formation de la cha&#238;ne pyr&#233;n&#233;enne)
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Juste au dessus de la limite (K/T), premi&#232;re s&#233;rie s&#233;dimentaire pal&#233;oc&#232;ne&lt;/p&gt;

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		<title>Taffoni (flysch gr&#233;seux de Jaizibel)</title>
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&lt;p&gt;Plusieurs magnifiques figures d'&#233;rosion le long du littoral &#224; la fronti&#232;re franco-espagnole&lt;/p&gt;

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		<title>Front d'alt&#233;ration flysch &#224; silex </title>
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&lt;p&gt;Alt&#233;rite importante surplombant les flysch &#224; silex de gu&#233;tary&lt;/p&gt;

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		<title>Flysch &#224; silex de Gu&#233;tary</title>
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&lt;p&gt;Formation du flysch &#224; silex de Gu&#233;tary, sur cette plage les s&#233;ries sont renvers&#233;es (granoclassement des turbidites, s&#233;diment grossier au top et fin, argilite &#224; la base). niveaux d'alt&#233;rites importants&lt;/p&gt;

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