{"id":19650,"date":"2015-12-03T00:00:00","date_gmt":"2015-12-03T00:00:00","guid":{"rendered":"https:\/\/lab.fabricadelandings.com.br\/portalsaofrancisco\/uncategorized\/placas-tectonicas-3\/"},"modified":"2026-09-01T15:24:03","modified_gmt":"2026-09-01T15:24:03","slug":"placas-tectonicas-3","status":"publish","type":"post","link":"https:\/\/lab.fabricadelandings.com.br\/portalsaofrancisco\/geografia-2\/placas-tectonicas-3\/","title":{"rendered":"Placas Tect\u00f4nicas"},"content":{"rendered":"\n<strong>As Placas Tect\u00f4nicas<\/strong>\n\nA camada externa da Terra, a litosfera, que consiste na crosta e no manto superior, \u00e9 dividida em uma colcha de retalhos de grandes placas tect\u00f4nicas que se movem lentamente umas em rela\u00e7\u00e3o \u00e0s outras. Existem 7-8 placas principais e muitas placas menores. Variando entre 0 a 100 mm por ano, o movimento de uma placa \u00e9 impulsionado por convec\u00e7\u00e3o no manto quente e viscoso subjacente.\n\nO planeta Terra possui uma grande diversidade em todas as suas caracter\u00edsticas, estas diferen\u00e7as s\u00e3o classificadas pelos geocientistas no decorrer do desenvolvimento das Geoci\u00eancias ou Ci\u00eancias Exatas, como a Geologia, a Geof\u00edsica, a Geografia, etc. Assim sendo, sabe-se que desde o seu n\u00facleo (parte inferior l\u00edquida), at\u00e9 a superf\u00edcie (parte superior s\u00f3lida) h\u00e1 grandes diferen\u00e7as, que se modificam ao longo do tempo geol\u00f3gico, configurando diferentes paisagens, dom\u00ednios e forma\u00e7\u00f5es.\n\nImersa nesta classifica\u00e7\u00e3o est\u00e3o as <strong>Placas Tect\u00f4nicas<\/strong>, mas o que de fato s\u00e3o essas estruturas? O que elas fazem? Onde fazem? Como fazem? E por que fazem?\n\nPara melhor compreender o que s\u00e3o placas tect\u00f4nicas, imagine que a Litosfera ou crosta da Terra(parte s\u00f3lida exterior da superf\u00edcie terrestre) n\u00e3o \u00e9 \u00fanica e igual em todo planeta, sendo, portanto, toda fatiada em algumas por\u00e7\u00f5es, que podem ser menores e maiores dependendo da regi\u00e3o, e que estas por\u00e7\u00f5es s\u00e3o separadas ou limitadas por zonas onde a din\u00e2mica geralmente \u00e9 intensa e com muita atividade geol\u00f3gica, ou seja, com terremotos e vulcanismos ou n\u00e3o, sendo comumente chamadas de zonas de diverg\u00eancias ou converg\u00eancia, que s\u00e3o respons\u00e1veis por formarem diferentes tipos de rochas e morfologias do relevo.\n\n<strong>Assim sendo, existem doze placas tect\u00f4nicas principais (grandes e pequenas), e s\u00e3o elas:<\/strong> Placa Indo-Australiana, Placa dos Cocos, Placa do Pac\u00edfico, Placa Eurasi\u00e1tica, Placa Norte Americana, Placa Ar\u00e1bica, Placa Sul-Americana, Placa Africana, Placa Caribenha e Placa de Nazca.\n<p class=\"imagem\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-128488 size-full\" title=\"Placas Tect\u00f4nicas\" src=\"https:\/\/lab.fabricadelandings.com.br\/portalsaofrancisco\/wp-content\/uploads\/2026\/08\/placas-tectonicas.jpg\" alt=\"Placas Tect\u00f4nicas\" width=\"450\" height=\"292\" \/><\/p>\nEssa din\u00e2mica descrita a cima tem como fonte principal o que os ge\u00f3logos chamam de <em>correntes de convec\u00e7\u00e3o<\/em>, que se refere ao material extremamente quente, tamb\u00e9m conhecido como magma, que \u00e9 formado na Astenosfera (camada abaixo da Litosfera) e que sobem em dire\u00e7\u00e3o \u00e0 Crosta, ocasionando o seu movimento e provocando atividades vulc\u00e2nicas e terremotos, formando as zonas de converg\u00eancia (uma placa se movimenta em dire\u00e7\u00e3o a outra placa). Neste caso ainda pode acontecer o que se chama de zona de subduc\u00e7\u00e3o, que \u00e9 quando uma placa se aprofunda sobre a outra, como se a mais densa estivesse engolindo a menos densa. Isso \u00e9 um exemplo do que ocorre quando a Placa de Nazca colida com a Placa Sul-Americana, formando a Cordilheira dos Andes.\n\nAl\u00e9m disso, h\u00e1 o movimento de converg\u00eancia entre duas placas continentais, o exemplo cl\u00e1ssico \u00e9 o choque entre as placas Euroasi\u00e1ticas e Ar\u00e1bicas, que acabam formando a cadeias de montanhas dos Himalaias, entre o Nepal, \u00cdndia, China e But\u00e3o.\n\nAo que se refere ao movimento de diverg\u00eancia de placas tect\u00f4nicas, tem-se a Cordilheira Meso Oce\u00e2nica abaixo dos oceanos \u00cdndico, Pac\u00edfico e Atl\u00e2ntico como caracter\u00edstica marcante. Neste movimento, as correntes de convec\u00e7\u00e3o agem em dire\u00e7\u00e3o contr\u00e1ria, acarretando em rupturas na crosta oce\u00e2nica, causando a constantemente a sua renova\u00e7\u00e3o, uma vez que possui din\u00e2mica complexas e intensa.\n\nGean Alef Cardoso\n","protected":false},"excerpt":{"rendered":"<p>Placas Tect\u00f4nicas, Tect\u00f4nia, Movimento, Causa, Terra, Brasil, Consequ\u00eancia, Localiza\u00e7\u00e3o, Tamanho, Terremotos, Tipos, Teoria, Placas Tect\u00f4nicas<\/p>\n","protected":false},"author":1,"featured_media":5489,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[52],"tags":[],"class_list":["post-19650","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-geografia-2"],"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v28.3 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Placas Tect\u00f4nicas - 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