{"id":276,"date":"2015-11-02T18:41:55","date_gmt":"2015-11-02T14:41:55","guid":{"rendered":"http:\/\/blogs.college-ledimitile.ac-reunion.fr\/?p=276"},"modified":"2016-11-14T18:45:37","modified_gmt":"2016-11-14T14:45:37","slug":"le-volcan-du-krakatoa","status":"publish","type":"post","link":"https:\/\/etab.ac-reunion.fr\/clg-le-dimitile-blog\/2015\/11\/02\/le-volcan-du-krakatoa\/","title":{"rendered":"Le volcan du Krakatoa"},"content":{"rendered":"

\"krakatoa-3\"<\/p>\n

\n
\n
\n
\n
\n
\n
\n

Nous sommes le 26 ao\u00fbt 1883 sur l\u2019\u00eele qui se situe entre Sumatra et Java en Indon\u00e9sie.
\nCe jour-l\u00e0, le volcan entre en \u00e9ruption.
\nLe bruit de l\u2019explosion se fait entendre jusqu\u2019en Australie tandis que l\u2019onde de choc arrive jusqu\u2019\u00e0 Madagascar.
\nD\u2019apr\u00e8s les chercheurs, cette explosion avait la puissance de 400 m\u00e9gatonnes de TNT (soit 20 000 fois Hiroshima). Non seulement l\u2019\u00e9ruption \u00e9tait puissante mais elle \u00e9tait \u00e9galement accompagn\u00e9e d\u2019orages et de pluie, ce qui ne faisait qu\u2019augmenter les flammes,de tsunamis et d\u2019explosions de magma qui atteignait les 200 m\u00e8tres cubes de lave !
\nCette \u00e9ruption causa des anomalies climatiques \u00e0 plusieurs endroits de la terre.
\nIl y eut 40 000 morts et l\u2019\u00eele fut engloutie par les eaux.<\/p>\n

\"krakatoa-2\"<\/p>\n

\"krakatoa-1024x350\"<\/p>\n

Article r\u00e9dig\u00e9 par Boris Hoarau (5\u00b0D)<\/strong><\/em><\/p>\n

Sources des images :<\/em>\u00a0<\/address>\n
http:\/\/www.krakatoaresources.com\/<\/address>\n
http:\/\/www.history.com<\/address>\n
http:\/\/volcanofacts101.weebly.com\/krakatoa.html<\/address>\n<\/div>\n<\/div>\n<\/div>\n<\/section>\n<\/div>\n<\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"

Nous sommes le 26 ao\u00fbt 1883 sur l\u2019\u00eele qui se situe entre Sumatra et Java en Indon\u00e9sie. Ce jour-l\u00e0, le volcan entre en \u00e9ruption. Le\u2026<\/p>\n

Lire la suite<\/i><\/a><\/p>\n","protected":false},"author":8105,"featured_media":85,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[8],"tags":[42],"class_list":["post-276","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-fous-de-volcan","tag-volcan"],"_links":{"self":[{"href":"https:\/\/etab.ac-reunion.fr\/clg-le-dimitile-blog\/wp-json\/wp\/v2\/posts\/276","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/etab.ac-reunion.fr\/clg-le-dimitile-blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/etab.ac-reunion.fr\/clg-le-dimitile-blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/etab.ac-reunion.fr\/clg-le-dimitile-blog\/wp-json\/wp\/v2\/users\/8105"}],"replies":[{"embeddable":true,"href":"https:\/\/etab.ac-reunion.fr\/clg-le-dimitile-blog\/wp-json\/wp\/v2\/comments?post=276"}],"version-history":[{"count":1,"href":"https:\/\/etab.ac-reunion.fr\/clg-le-dimitile-blog\/wp-json\/wp\/v2\/posts\/276\/revisions"}],"predecessor-version":[{"id":277,"href":"https:\/\/etab.ac-reunion.fr\/clg-le-dimitile-blog\/wp-json\/wp\/v2\/posts\/276\/revisions\/277"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/etab.ac-reunion.fr\/clg-le-dimitile-blog\/wp-json\/wp\/v2\/media\/85"}],"wp:attachment":[{"href":"https:\/\/etab.ac-reunion.fr\/clg-le-dimitile-blog\/wp-json\/wp\/v2\/media?parent=276"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/etab.ac-reunion.fr\/clg-le-dimitile-blog\/wp-json\/wp\/v2\/categories?post=276"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/etab.ac-reunion.fr\/clg-le-dimitile-blog\/wp-json\/wp\/v2\/tags?post=276"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}