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U. Point-chaud-À-proximité-d-'une-marge-continentale and ?. ???, Une hypothèse réfutée : l'influence de la ceinture orogénique alpine ?..? 1.1.1.2. Quelques rappels sur la géodynamique interne des points chauds ?..??. 1.1.1.3. Les arguments en faveur d'un point chaud sous les Iles Canaries ????

. Les??, massifs anciens" : la cessation de l'activité volcanique???

. Un-témoin-unique, Agaete (Gran Canaria)?????.. 2.1.1.1. Un dispositif topographique peu commun?????????.???. 2.1.1.2

L. , C. Nueva, L. La-caldera-de-taburiente, and . Palma???, ??. 2.2.1.1. Les étapes de la construction du volcan bouclier de Taburiente??.??. 2.2.1.2. Le problème de l'origine de La Caldera de Taburiente???????? 2.2.1.3. L'instabilité récurrente des flancs sud-ouest de La Palma??????? 2.2.1.4. Les marqueurs volcaniques de la formation de la Caldera de Taburiente? 2.2.1.5. L'évolution morphogénique

L. Le-remplissage-volcanique-d-'une-cicatrice-de-déstabilisation-À and . Gomera??, ? 2.2.2.1. La destruction des flancs nord du bouclier : le glissement Garajonay?..? 2.2.2.2. Typologie et signification des brèches de la surface de glissement??.?. 2.2.2.3. L'évolution spatio-temporelle du remplissage volcanique de la cicatrice

. ?. Une-approche-quantitative-des-barrancos???????????? and . ???, Discussion : apports et limites d'une approche quantitative??

?. Renouvellements-de-surface-et-inversion-de-relief and . ????, 3.1.2.1. Les premiers barrancos de La Gomera?????????..?.???. 3.1.2.2. Les flancs sud de Las Cañadas : un relief à géométrie variable??

L. 'article-de and J. L. Schneider, cité page 327, traite de la corrélation entre la sédimentation du talus volcanoclastique et les principales phases volcaniques du nord de Gran Canaria. Ayant travaillé en collaboration avec J.L. Schneider, nous y ajoutons des remarques personnelles sur l'évolution morphologique et sur les rythmes d'érosion estimés précédemment, Page, vol.327, 1997.

M. Viñuela, Catedrático Cristalografia y Mineralogia, Física- Geologia