{"id":455,"date":"2025-01-16T09:44:23","date_gmt":"2025-01-16T08:44:23","guid":{"rendered":"https:\/\/mruizsvt.fr\/?page_id=455"},"modified":"2025-01-16T09:44:38","modified_gmt":"2025-01-16T08:44:38","slug":"2-2-la-structure-des-plaques-en-surfaces","status":"publish","type":"page","link":"https:\/\/mruizsvt.fr\/index.php\/4-eme\/chapitre-2-les-seismes-et-la-tectonique-des-plaques\/2-2-la-structure-des-plaques-en-surfaces\/","title":{"rendered":"2.2 La structure des plaques en surfaces"},"content":{"rendered":"\n<blockquote class=\"wp-block-quote has-text-align-center is-layout-flow wp-block-quote-is-layout-flow\">\n<p>Exercice<\/p>\n<\/blockquote>\n\n\n\n<div data-wp-interactive=\"core\/file\" class=\"wp-block-file\"><object data-wp-bind--hidden=\"!state.hasPdfPreview\" hidden class=\"wp-block-file__embed\" data=\"https:\/\/mruizsvt.fr\/wp-content\/uploads\/2025\/01\/Activite-2-structure-plaque-en-surface.pdf\" type=\"application\/pdf\" style=\"width:100%;height:600px\" aria-label=\"Contenu embarqu\u00e9 Activit\u00e9 2 structure plaque en surface.\"><\/object><a id=\"wp-block-file--media-aee22646-7328-4ccd-b1a9-17bf84bf2e05\" href=\"https:\/\/mruizsvt.fr\/wp-content\/uploads\/2025\/01\/Activite-2-structure-plaque-en-surface.pdf\">Activit\u00e9 2 structure plaque en surface<\/a><a href=\"https:\/\/mruizsvt.fr\/wp-content\/uploads\/2025\/01\/Activite-2-structure-plaque-en-surface.pdf\" class=\"wp-block-file__button wp-element-button\" download aria-describedby=\"wp-block-file--media-aee22646-7328-4ccd-b1a9-17bf84bf2e05\">T\u00e9l\u00e9charger<\/a><\/div>\n\n\n\n<blockquote class=\"wp-block-quote is-layout-flow wp-block-quote-is-layout-flow\">\n<p class=\"has-text-align-center\">Correction<\/p>\n<\/blockquote>\n\n\n\n<p>Correction&nbsp;:<\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li>Les volcans sont r\u00e9partis\u00a0:<br>Au bord des continents, sur les c\u00f4tes<br>Au milieu des oc\u00e9ans<br>Dans les zones montagneuses<\/li>\n<\/ol>\n\n\n\n<p>2. Les s\u00e9ismes sont r\u00e9partis\u00a0:<br>    Au bord des continents, sur les c\u00f4tes<br>    Au milieu des oc\u00e9ans<br>    Dans les zones montagneuses<\/p>\n\n\n\n<p>3. Les s\u00e9ismes et les volcans sont quasiment aux m\u00eames emplacements<\/p>\n\n\n\n<p>4. Les s\u00e9ismes et les volcans sont r\u00e9partis aux m\u00eames emplacements, ils forment de grands alignements de zones tr\u00e8s actives entourant des zones tr\u00e8s calmes.<\/p>\n\n\n\n<blockquote class=\"wp-block-quote is-layout-flow wp-block-quote-is-layout-flow\">\n<p class=\"has-text-align-center\">Bilan<\/p>\n<\/blockquote>\n\n\n\n<p class=\"has-accent-3-color has-text-color has-link-color wp-elements-72a45c5a54f579184a46c4e6aec1609b\">Les plaques sont d\u00e9limit\u00e9es en surface par des zones tr\u00e8s actives en s\u00e9ismes et en volcan, ces zones sont appel\u00e9es limites de plaques. A la diff\u00e9rence au milieu de ces plaques il y a tr\u00e8s peu d\u2019activit\u00e9 sismique et volcanique.<\/p>\n\n\n\n<p class=\"has-accent-3-color has-text-color has-link-color wp-elements-3385c73d8d1edb35b0d910fdcc36bd1f\">Ces plaques sont soit oc\u00e9anique, soit oc\u00e9anique et continentale.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"850\" height=\"600\" src=\"https:\/\/mruizsvt.fr\/wp-content\/uploads\/2025\/01\/Carte-plaque.png\" alt=\"\" class=\"wp-image-456\" srcset=\"https:\/\/mruizsvt.fr\/wp-content\/uploads\/2025\/01\/Carte-plaque.png 850w, https:\/\/mruizsvt.fr\/wp-content\/uploads\/2025\/01\/Carte-plaque-300x212.png 300w, https:\/\/mruizsvt.fr\/wp-content\/uploads\/2025\/01\/Carte-plaque-768x542.png 768w\" sizes=\"auto, (max-width: 850px) 100vw, 850px\" \/><\/figure>\n\n\n\n<p><strong><br><\/strong><\/p>\n\n\n\n<p><\/p>\n\n\n\n<p><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Exercice Correction Correction&nbsp;: 2. Les s\u00e9ismes sont r\u00e9partis\u00a0: Au bord des continents, sur les c\u00f4tes Au milieu des oc\u00e9ans Dans les zones montagneuses 3. Les s\u00e9ismes et les volcans sont quasiment aux m\u00eames emplacements 4. Les s\u00e9ismes et les volcans sont r\u00e9partis aux m\u00eames emplacements, ils forment de grands alignements de zones tr\u00e8s actives entourant [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":142,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-455","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/mruizsvt.fr\/index.php\/wp-json\/wp\/v2\/pages\/455","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/mruizsvt.fr\/index.php\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/mruizsvt.fr\/index.php\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/mruizsvt.fr\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/mruizsvt.fr\/index.php\/wp-json\/wp\/v2\/comments?post=455"}],"version-history":[{"count":1,"href":"https:\/\/mruizsvt.fr\/index.php\/wp-json\/wp\/v2\/pages\/455\/revisions"}],"predecessor-version":[{"id":458,"href":"https:\/\/mruizsvt.fr\/index.php\/wp-json\/wp\/v2\/pages\/455\/revisions\/458"}],"up":[{"embeddable":true,"href":"https:\/\/mruizsvt.fr\/index.php\/wp-json\/wp\/v2\/pages\/142"}],"wp:attachment":[{"href":"https:\/\/mruizsvt.fr\/index.php\/wp-json\/wp\/v2\/media?parent=455"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}