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        <Text language="eng">&lt;p&gt;The Bay of Lannion underwent a geological mapping programme between 2005 and 2009. The previously unpublished results are presented as seven 1:20000 scale maps and an explanatory booklet. They could serve as a reference state in the various local on-going or forthcoming projects in both the scientific and applied fields. The huge diversity of sediments on the sea bottom, closely related to the hydrodynamics, proves the wealth of this bay. This atlas will appeal to professionals, teachers, developers, public decision-makers and anyone interested and concerned about their working or leisure setting.&lt;/p&gt;</Text>
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        <Text>La baie de Lannion a fait l'objet d’un programme de cartographie géologique entre 2005 et 2009. Les résultats, tous inédits, sont présentés sous la forme de sept cartes à l'échelle 1/20 000 et d'un livret d'accompagnement.</Text>
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        <Text>&lt;p&gt;&lt;b&gt;Introduction&lt;/b&gt;&lt;/p&gt;&lt;p&gt;&lt;br /&gt;&lt;b&gt;Chapitre I - Pr&amp;eacute;sentation g&amp;eacute;n&amp;eacute;rale de la baie de Lannion&lt;/b&gt;&lt;br /&gt;Pr&amp;eacute;sentation g&amp;eacute;n&amp;eacute;rale&lt;br /&gt;Cadre g&amp;eacute;ologique g&amp;eacute;n&amp;eacute;ral&lt;br /&gt;G&amp;eacute;omorphologie littorale&lt;br /&gt;Nature des fonds&lt;br /&gt;R&amp;eacute;gime hydrodynamique&lt;br /&gt;&lt;br /&gt;&lt;b&gt;Chapitre II - Moyens de reconnaissance en mer, travaux r&amp;eacute;alis&amp;eacute;s&lt;/b&gt;&lt;br /&gt;Moyens utilisant l&amp;rsquo;acoustique&lt;br /&gt;Outils de pr&amp;eacute;l&amp;egrave;vement d&amp;rsquo;&amp;eacute;chantillons&lt;br /&gt;Le syst&amp;egrave;me de positionnement&lt;br /&gt;Les travaux r&amp;eacute;alis&amp;eacute;s en mer&lt;br /&gt;Autres donn&amp;eacute;es utilis&amp;eacute;es&lt;br /&gt;&lt;br /&gt;&lt;b&gt;Chapitre III - G&amp;eacute;ologie du substratum&lt;/b&gt;&lt;/p&gt;&lt;p&gt;&lt;br /&gt;&lt;b&gt;Chapitre IV &amp;ndash; Remplissage s&amp;eacute;dimentaire quaternaire&lt;/b&gt;&lt;br /&gt;Morphologie du toit du substratum rocheux&lt;br /&gt;Analyse du pal&amp;eacute;or&amp;eacute;seau&lt;br /&gt;Les diff&amp;eacute;rentes unit&amp;eacute;s &amp;ldquo;sismiques&amp;rdquo; de comblement du pal&amp;eacute;or&amp;eacute;seau&lt;br /&gt;Identification des ensembles s&amp;eacute;dimentaires&lt;br /&gt;Gen&amp;egrave;se du pal&amp;eacute;or&amp;eacute;seau de la baie de Lannion&lt;br /&gt;Remplissage du pal&amp;eacute;or&amp;eacute;seau et pal&amp;eacute;o-environnements de d&amp;eacute;p&amp;ocirc;t&lt;br /&gt;&lt;br /&gt;&lt;b&gt;Chapitre V - Morphologie des fonds, nature et r&amp;eacute;partition des formations marines actuelles&lt;/b&gt;&lt;br /&gt;Morpho-bathym&amp;eacute;trie&lt;br /&gt;Nature et r&amp;eacute;partition des formations superficielles&lt;br /&gt;Dynamique des s&amp;eacute;diments&lt;br /&gt;Synth&amp;egrave;se r&amp;eacute;gionale sur la connaissance de la nature des fonds marins&lt;br /&gt;Comparaison avec la carte ancienne de nature des fonds (1973)&lt;br /&gt;&lt;br /&gt;&lt;b&gt;Conclusion&lt;/b&gt;&lt;/p&gt;&lt;p&gt;&lt;br /&gt;&lt;b&gt;R&amp;eacute;f&amp;eacute;rences bibliographiques&lt;/b&gt;&lt;/p&gt;</Text>
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        <Text language="fre">&lt;p&gt;La baie de Lannion a fait l&amp;#39;objet d&amp;rsquo;un programme de cartographie g&amp;eacute;ologique entre 2005 et 2009. Les r&amp;eacute;sultats, tous in&amp;eacute;dits, sont pr&amp;eacute;sent&amp;eacute;s sous la forme de sept cartes &amp;agrave; l&amp;#39;&amp;eacute;chelle 1/20 000 et d&amp;#39;un livret d&amp;#39;accompagnement. Ils pourront servir d&amp;rsquo;&amp;eacute;tat de r&amp;eacute;f&amp;eacute;rence dans les diff&amp;eacute;rents projets locaux en cours ou &amp;agrave; venir, tant dans le domaine scientifique qu&amp;#39;appliqu&amp;eacute;. La grande diversit&amp;eacute; des s&amp;eacute;diments sur le fond, en relation &amp;eacute;troite avec l&amp;rsquo;hydrodynamisme, atteste de la richesse de cette baie. Cet atlas int&amp;eacute;ressera les professionnels, les enseignants, les am&amp;eacute;nageurs, les d&amp;eacute;cideurs publics et tous ceux qui se pr&amp;eacute;occupent de leur cadre de travail ou de loisir.&lt;/p&gt;</Text>
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        <Text language="fre">&lt;p&gt;La baie de Lannion a fait l&amp;#39;objet d&amp;rsquo;un programme de cartographie g&amp;eacute;ologique entre 2005 et 2009. Les r&amp;eacute;sultats, tous in&amp;eacute;dits, sont pr&amp;eacute;sent&amp;eacute;s sous la forme de sept cartes &amp;agrave; l&amp;#39;&amp;eacute;chelle 1/20 000 et d&amp;#39;un livret d&amp;#39;accompagnement. Ils pourront servir d&amp;rsquo;&amp;eacute;tat de r&amp;eacute;f&amp;eacute;rence dans les diff&amp;eacute;rents projets locaux en cours ou &amp;agrave; venir, tant dans le domaine scientifique qu&amp;#39;appliqu&amp;eacute;. La grande diversit&amp;eacute; des s&amp;eacute;diments sur le fond, en relation &amp;eacute;troite avec l&amp;rsquo;hydrodynamisme, atteste de la richesse de cette baie. Cet atlas int&amp;eacute;ressera les professionnels, les enseignants, les am&amp;eacute;nageurs, les d&amp;eacute;cideurs publics et tous ceux qui se pr&amp;eacute;occupent de leur cadre de travail ou de loisir.&lt;/p&gt;</Text>
        <Text language="eng">&lt;p&gt;The Bay of Lannion underwent a geological mapping programme between 2005 and 2009. The previously unpublished results are presented as seven 1:20000 scale maps and an explanatory booklet. They could serve as a reference state in the various local on-going or forthcoming projects in both the scientific and applied fields. The huge diversity of sediments on the sea bottom, closely related to the hydrodynamics, proves the wealth of this bay. This atlas will appeal to professionals, teachers, developers, public decision-makers and anyone interested and concerned about their working or leisure setting.&lt;/p&gt;</Text>
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        <Text>&lt;p&gt;&lt;b&gt;Introduction&lt;/b&gt;&lt;/p&gt;&lt;p&gt;&lt;br /&gt;&lt;b&gt;Chapitre I - Pr&amp;eacute;sentation g&amp;eacute;n&amp;eacute;rale de la baie de Lannion&lt;/b&gt;&lt;br /&gt;Pr&amp;eacute;sentation g&amp;eacute;n&amp;eacute;rale&lt;br /&gt;Cadre g&amp;eacute;ologique g&amp;eacute;n&amp;eacute;ral&lt;br /&gt;G&amp;eacute;omorphologie littorale&lt;br /&gt;Nature des fonds&lt;br /&gt;R&amp;eacute;gime hydrodynamique&lt;br /&gt;&lt;br /&gt;&lt;b&gt;Chapitre II - Moyens de reconnaissance en mer, travaux r&amp;eacute;alis&amp;eacute;s&lt;/b&gt;&lt;br /&gt;Moyens utilisant l&amp;rsquo;acoustique&lt;br /&gt;Outils de pr&amp;eacute;l&amp;egrave;vement d&amp;rsquo;&amp;eacute;chantillons&lt;br /&gt;Le syst&amp;egrave;me de positionnement&lt;br /&gt;Les travaux r&amp;eacute;alis&amp;eacute;s en mer&lt;br /&gt;Autres donn&amp;eacute;es utilis&amp;eacute;es&lt;br /&gt;&lt;br /&gt;&lt;b&gt;Chapitre III - G&amp;eacute;ologie du substratum&lt;/b&gt;&lt;/p&gt;&lt;p&gt;&lt;br /&gt;&lt;b&gt;Chapitre IV &amp;ndash; Remplissage s&amp;eacute;dimentaire quaternaire&lt;/b&gt;&lt;br /&gt;Morphologie du toit du substratum rocheux&lt;br /&gt;Analyse du pal&amp;eacute;or&amp;eacute;seau&lt;br /&gt;Les diff&amp;eacute;rentes unit&amp;eacute;s &amp;ldquo;sismiques&amp;rdquo; de comblement du pal&amp;eacute;or&amp;eacute;seau&lt;br /&gt;Identification des ensembles s&amp;eacute;dimentaires&lt;br /&gt;Gen&amp;egrave;se du pal&amp;eacute;or&amp;eacute;seau de la baie de Lannion&lt;br /&gt;Remplissage du pal&amp;eacute;or&amp;eacute;seau et pal&amp;eacute;o-environnements de d&amp;eacute;p&amp;ocirc;t&lt;br /&gt;&lt;br /&gt;&lt;b&gt;Chapitre V - Morphologie des fonds, nature et r&amp;eacute;partition des formations marines actuelles&lt;/b&gt;&lt;br /&gt;Morpho-bathym&amp;eacute;trie&lt;br /&gt;Nature et r&amp;eacute;partition des formations superficielles&lt;br /&gt;Dynamique des s&amp;eacute;diments&lt;br /&gt;Synth&amp;egrave;se r&amp;eacute;gionale sur la connaissance de la nature des fonds marins&lt;br /&gt;Comparaison avec la carte ancienne de nature des fonds (1973)&lt;br /&gt;&lt;br /&gt;&lt;b&gt;Conclusion&lt;/b&gt;&lt;/p&gt;&lt;p&gt;&lt;br /&gt;&lt;b&gt;R&amp;eacute;f&amp;eacute;rences bibliographiques&lt;/b&gt;&lt;/p&gt;</Text>
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