{"id":308,"date":"2021-03-25T16:37:35","date_gmt":"2021-03-25T15:37:35","guid":{"rendered":"https:\/\/www.vulcania.com\/science\/?page_id=308"},"modified":"2023-03-22T10:04:37","modified_gmt":"2023-03-22T09:04:37","slug":"eruption-strombolienne","status":"publish","type":"page","link":"https:\/\/www.vulcania.com\/science\/volcans\/differents-types-deruptions\/eruption-strombolienne\/","title":{"rendered":"\u00c9ruption strombolienne"},"content":{"rendered":"

[vc_row el_class=\u00a0\u00bbbloc-titre\u00a0\u00bb][vc_column width=\u00a0\u00bb1\/12″][\/vc_column][vc_column width=\u00a0\u00bb10\/12″][vc_row_inner content_placement=\u00a0\u00bbmiddle\u00a0\u00bb][vc_column_inner width=\u00a0\u00bb1\/4″][vc_single_image image=\u00a0\u00bb309″ img_size=\u00a0\u00bbfull\u00a0\u00bb][\/vc_column_inner][vc_column_inner width=\u00a0\u00bb3\/4″][vc_column_text]Type d\u00e9fini sur l\u2019\u00eele de Stromboli, en Italie du Sud, les \u00e9ruptions stromboliennes alternent phases explosives et phases effusives. Elles sont caract\u00e9ris\u00e9es par l\u2019\u00e9jection rythmique de lambeaux de lave propuls\u00e9s par les gaz volcaniques. Parfois, le crat\u00e8re d\u00e9borde d\u2019une lave fluide qui alimente des coul\u00e9es. L\u2019\u00e9ruption dure de quelques jours \u00e0 quelques mois, puis s\u2019arr\u00eate. Le c\u00f4ne est compos\u00e9 d\u2019une succession de strates riches en cendres et en bombes volcaniques et de strates form\u00e9es par les coul\u00e9es de lave refroidies.<\/p>\n

La plupart des jeunes volcans de la Cha\u00eene des Puys (Massif central fran\u00e7ais) sont n\u00e9s \u00e0 la suite de ce type d\u2019\u00e9ruption. Chaque nouvelle arriv\u00e9e de magma en surface a fait appara\u00eetre un nouveau volcan. Ainsi, entre -100 000 ans et -6 700 ans, quelques dizaines de c\u00f4nes de scories<\/a> entour\u00e9s de leurs coul\u00e9es se sont construits.<\/p>\n

Paradoxalement, le volcan de r\u00e9f\u00e9rence, le Stromboli, est tout \u00e0 fait atypique. Il est en effet actif de mani\u00e8re permanente depuis au moins 2 700 ans\u2026[\/vc_column_text][\/vc_column_inner][\/vc_row_inner][\/vc_column][vc_column width=\u00a0\u00bb1\/12″][\/vc_column][\/vc_row][vc_row][vc_column width=\u00a0\u00bb1\/12″][\/vc_column][vc_column width=\u00a0\u00bb10\/12″][vc_column_text]<\/p>\n

Les autres types d’\u00e9ruptions :<\/h3>\n

[\/vc_column_text][vc_basic_grid post_type=\u00a0\u00bbpage\u00a0\u00bb max_items=\u00a0\u00bb10″ element_width=\u00a0\u00bb3″ item=\u00a0\u00bb573″ grid_id=\u00a0\u00bbvc_gid:1679475847806-4ceb742c-a229-10″ taxonomies=\u00a0\u00bb17″][\/vc_column][vc_column width=\u00a0\u00bb1\/12″][\/vc_column][\/vc_row][vc_row][vc_column]

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Exp\u00e9rimentez \u00e0 Vulcania<\/h4><\/span><\/span>\n<\/div>
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Volcans, comment \u00e7a marche ?<\/h3>\n

O\u00f9 et pourquoi les volcans se forment-ils ? Avec l'atelier \"Volcans, comment \u00e7a marche ?\" du Coin des exp\u00e9riences, levez le voile sur les secrets du volcanisme !<\/p>\n\n\t\t<\/div>\n\t<\/div>\n

En savoir plus sur les \"Ateliers des volcans\"<\/a><\/div><\/div><\/div><\/div>
<\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div>[\/vc_column][\/vc_row]<\/p>\n<\/div>","protected":false},"excerpt":{"rendered":"Exp\u00e9rimentez \u00e0 Vulcania Volcans, comment \u00e7a marche ? O\u00f9 et pourquoi les volcans se forment-ils ? Avec l'atelier \"Volcans, comment \u00e7a marche ?\" du Coin des exp\u00e9riences, levez le voile sur les secrets du volcanisme ! En savoir plus sur les \"Ateliers des volcans\"","protected":false},"author":4,"featured_media":755,"parent":223,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"tags":[17],"acf":[],"yoast_head":"\nLe Stromboli et les \u00e9ruptions stromboliennes<\/title>\n<meta name=\"description\" content=\"Caract\u00e9ris\u00e9es par des phases explosives et des phases effusives, ces \u00e9ruptions ont \u00e9t\u00e9 observ\u00e9es sur l'\u00eele de Stromboli. 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