{"id":706,"date":"2015-10-25T18:47:13","date_gmt":"2015-10-25T18:47:13","guid":{"rendered":"https:\/\/vesnajanko.eu\/?page_id=706"},"modified":"2025-12-16T18:15:01","modified_gmt":"2025-12-16T17:15:01","slug":"6-13-reljef-u-pokretu","status":"publish","type":"page","link":"https:\/\/vesnajanko.eu\/?page_id=706","title":{"rendered":"Reljef Azije"},"content":{"rendered":"\n<p class=\"has-text-align-right\"><a href=\"https:\/\/www.scribblemaps.com\/maps\/view\/Azija\/Azija\" target=\"_blank\" rel=\"noopener noreferrer\"><br><input class=\"button\" type=\"button\" value=\"Karta Azije\"><br><\/a><\/p>\n\n\n\n<p><span style=\"text-decoration: underline;\">Uvod<\/span><\/p>\n\n\n\n<p><a rel=\"noopener noreferrer\" href=\"https:\/\/www.businessinsider.com\/how-earth-will-look-250-million-years-map-animation-2017-9?utm_content=buffer27137&amp;utm_medium=social&amp;utm_source=facebook.com&amp;utm_campaign=buffer\" target=\"_blank\">Zemlja za 250 mil. godina<\/a><\/p>\n\n\n\n<div style=\"height:47px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<p><span style=\"text-decoration: underline;\">Obrada i ponavljanje<\/span><\/p>\n\n\n\n<p>LITOSFERNE PLO\u010cE<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><a href=\"http:\/\/youtu.be\/ryrXAGY1dmE\" target=\"_blank\" rel=\"noopener noreferrer\">http:\/\/youtu.be\/ryrXAGY1dmE<\/a><\/li>\n\n\n\n<li><a href=\"https:\/\/youtu.be\/cQVoSyVu9rk\" target=\"_blank\" rel=\"noopener noreferrer\">https:\/\/youtu.be\/cQVoSyVu9rk<\/a><\/li>\n<\/ul>\n\n\n\n<ul class=\"wp-block-list\">\n<li>\u017divot na rubu litosfernih plo\u010da\n<ul class=\"wp-block-list\">\n<li><a href=\"https:\/\/youtu.be\/chbbiSCczB8\" target=\"_blank\" rel=\"noopener noreferrer\">https:\/\/youtu.be\/chbbiSCczB8<\/a><\/li>\n\n\n\n<li><a href=\"http:\/\/youtu.be\/Gbd1FcuLJLQ\" target=\"_blank\" rel=\"noopener noreferrer\">http:\/\/youtu.be\/Gbd1FcuLJLQ<\/a><\/li>\n<\/ul>\n<\/li>\n\n\n\n<li>Koliko je dubok ocean?\n<ul class=\"wp-block-list\">\n<li><a href=\"https:\/\/youtu.be\/UwVNkfCov1k\" target=\"_blank\" rel=\"noopener noreferrer\">https:\/\/youtu.be\/UwVNkfCov1k<\/a><\/li>\n<\/ul>\n<\/li>\n<\/ul>\n\n\n\n<div style=\"height:40px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<p class=\"has-pale-ocean-gradient-background has-background\"><strong><a href=\"https:\/\/docs.google.com\/presentation\/d\/e\/2PACX-1vT9ubaGcPTFc4PkSr1otUfp8kfz_aqhqPofVmEDSi6hl-JK3r303yckFXX70KQLmKWBeNLaggad0sgy\/pub?start=false&amp;loop=false&amp;delayms=3000\" target=\"_blank\" rel=\"noreferrer noopener\">Prezentacija<\/a><\/strong><\/p>\n\n\n\n<iframe loading=\"lazy\" src=\"https:\/\/docs.google.com\/presentation\/d\/e\/2PACX-1vT9ubaGcPTFc4PkSr1otUfp8kfz_aqhqPofVmEDSi6hl-JK3r303yckFXX70KQLmKWBeNLaggad0sgy\/pubembed?start=false&#038;loop=false&#038;delayms=3000\" frameborder=\"0\" width=\"960\" height=\"569\" allowfullscreen=\"true\" mozallowfullscreen=\"true\" webkitallowfullscreen=\"true\"><\/iframe>\n\n\n\n<div style=\"height:36px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<p><a href=\"https:\/\/www.scribblemaps.com\/maps\/view\/Azija\/Azija\" target=\"_blank\" rel=\"noopener noreferrer\">Karta Azije<\/a><\/p>\n\n\n\n<p><a href=\"http:\/\/www.purposegames.com\/game\/reljef-azije-planine-gorja-visoravni\" target=\"_blank\" rel=\"noopener noreferrer\">Vje\u017eba na karti<\/a>.<\/p>\n\n\n\n<h4 class=\"wp-block-heading has-pale-cyan-blue-background-color has-background\">Geobilje\u0161ke<\/h4>\n\n\n\n<p class=\"has-text-align-center\"><span style=\"text-decoration: underline;\">Reljef Azije<\/span><\/p>\n\n\n\n<p>\u2013&nbsp;<strong>pomicanje litosfernih plo\u010da<\/strong>&nbsp;utje\u010du na oblikovanje reljefa Azije<\/p>\n\n\n\n<p>\u2013 seizmologija \u2013 istra\u017euje potrese i njihove posljedice \u2013 seizmograf (mjeri ja\u010dinu potresa)<\/p>\n\n\n\n<p>\u2013 vulkanologija \u2013 istra\u017euje vulkane i vulkanske pojave<\/p>\n\n\n\n<p>\u2013 \u201c<strong>pacifi\u010dki vatreni prsten<\/strong>\u201d \u2013 niz vulkanskih i sezmi\u010dkih aktivnosti du\u017e tihooceanske litosferne plo\u010de<\/p>\n\n\n\n<p>\u2013&nbsp;<strong>tsunami<\/strong>&nbsp;\u2013 morski valovi izazvani podmorskim potresom<\/p>\n\n\n\n<figure class=\"wp-block-table\"><table><tbody><tr><td><strong>reljefni oblici<\/strong><\/td><td><strong>obilje\u017eja<\/strong><\/td><td><strong>primjeri u Aziji<\/strong><\/td><\/tr><tr><td>mlade nabrane planine<\/td><td>visoke i strme<\/td><td>Himalaja, Karakorum, Hinduku\u0161, Pamir<\/td><\/tr><tr><td>visoravni<\/td><td>ravnice iznad 200 m<\/td><td>Tibet, Anatolija, Iranska visoravan<\/td><\/tr><tr><td>staro gromadno gorje<\/td><td>sni\u017eene, blagih vrhova<\/td><td>Zapadni i Isto\u010dni Gati, Ural, Srednjesibirsko gorje<\/td><\/tr><tr><td>prastari \u0161titovi i platforme<\/td><td>sni\u017eena dugim djelovanjem vanjskih procesa<\/td><td>Dekan, Arapski \u0161tit, Sibirska platforma i \u0161tit<\/td><\/tr><tr><td>nizine<\/td><td>ravnice do 200 m<\/td><td>Mezopotmija, Hindustan, Velika kineska nizina<\/td><\/tr><tr><td>depresije<\/td><td>ispod razine mora<\/td><td>Mrtvo more<\/td><\/tr><tr><td>dubokomorski jarci<\/td><td>na rubovima litosfernih plo\u010da<\/td><td>Marijanska brazda, Filipinska brazda<\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n<figure class=\"wp-block-table\"><table><tbody><tr><td><strong>Prednosti \u017eivota uz vulkan<\/strong><\/td><td><strong>Nedostaci \u017eivota uz vulkan<\/strong><\/td><\/tr><tr><td>plodno tlo, izvori tople vode&nbsp;<\/td><td>opasnost od erupcija, potresa, tsunamija<\/td><\/tr><\/tbody><\/table><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>Uvod Zemlja za 250 mil. godina Obrada i ponavljanje LITOSFERNE PLO\u010cE Prezentacija Karta Azije Vje\u017eba na karti. Geobilje\u0161ke Reljef Azije \u2013&nbsp;pomicanje litosfernih plo\u010da&nbsp;utje\u010du na oblikovanje reljefa Azije \u2013 seizmologija \u2013 istra\u017euje potrese i njihove posljedice \u2013 seizmograf (mjeri ja\u010dinu potresa) \u2013 vulkanologija \u2013 istra\u017euje vulkane i vulkanske pojave \u2013 \u201cpacifi\u010dki&#8230; <a href=\"https:\/\/vesnajanko.eu\/?page_id=706\" class=\"readmore\">Vi\u0161e<span class=\"screen-reader-text\">&#8220;Reljef Azije&#8221;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":7242,"menu_order":2,"comment_status":"closed","ping_status":"closed","template":"templates\/page-full-width.php","meta":{"footnotes":""},"class_list":["post-706","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/vesnajanko.eu\/index.php?rest_route=\/wp\/v2\/pages\/706","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/vesnajanko.eu\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/vesnajanko.eu\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/vesnajanko.eu\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/vesnajanko.eu\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=706"}],"version-history":[{"count":35,"href":"https:\/\/vesnajanko.eu\/index.php?rest_route=\/wp\/v2\/pages\/706\/revisions"}],"predecessor-version":[{"id":10209,"href":"https:\/\/vesnajanko.eu\/index.php?rest_route=\/wp\/v2\/pages\/706\/revisions\/10209"}],"up":[{"embeddable":true,"href":"https:\/\/vesnajanko.eu\/index.php?rest_route=\/wp\/v2\/pages\/7242"}],"wp:attachment":[{"href":"https:\/\/vesnajanko.eu\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=706"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}