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        <BiographicalNote language="eng">&lt;p&gt;Claude Augris, a geologist at Ifremer, is in charge of geological mapping of the coastal marine field and studies on aggregates. In this context, he coordinates the provision of advice and opinions on behalf of State services.&lt;/p&gt;</BiographicalNote>
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        <Text language="fre">&lt;p&gt;L&amp;#39;originalit&amp;eacute; de cette cartographie r&amp;eacute;side dans la caract&amp;eacute;risation pr&amp;eacute;cise des diff&amp;eacute;rentes &amp;quot;rocs&amp;quot;. Les roches de Saint-Laurent et de Torreilles ne constituent qu&amp;#39;un seul et m&amp;ecirc;me ensemble. Le &amp;quot;rocher&amp;quot; de Saint-Cyprien est compos&amp;eacute; en majorit&amp;eacute; de sables grossiers et de graviers&amp;nbsp;; de m&amp;ecirc;me, le &amp;quot;rocher&amp;quot; de la T&amp;ecirc;t est compos&amp;eacute; par un &amp;eacute;pandage de s&amp;eacute;diments grossiers localement envas&amp;eacute;s.&lt;/p&gt;</Text>
        <Text language="eng">&lt;p&gt;Carte des formations superficielles sous-marines entre Port-Barcar&amp;egrave;s et Saint-Cyprien (Pyr&amp;eacute;n&amp;eacute;es-Orientales)&lt;/p&gt;</Text>
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        <Text>L'originalité de cette cartographie réside dans la caractérisation précise des différentes "rocs". Les roches de Saint-Laurent et de Torreilles ne constituent qu'un seul et même ensemble. Le "rocher" de Saint-Cyprien est composé en majorité de sables grossiers et de graviers ; de même, le "rocher" de la Têt est composé par un épandage de sédiments grossiers localement envasés.</Text>
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