{"id":132,"date":"2024-04-04T06:11:47","date_gmt":"2024-04-04T03:11:47","guid":{"rendered":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/kivimid\/"},"modified":"2024-04-04T06:13:02","modified_gmt":"2024-04-04T03:13:02","slug":"kivimid","status":"publish","type":"page","link":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/kivimid\/","title":{"rendered":"Kivimid"},"content":{"rendered":"<p>\n\t<b>Tekkest l\u00e4htudes<\/b>\u00a0eristatakse kolme kivimite suurt r\u00fchma (skeem 1 ja 2):\n<\/p>\n<p>\n\t\u00a0\n<\/p>\n<ul>\n<li>\n<p>\n\t\t\t<a data-url=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/tardkivimid\" href=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/tardkivimid\" target=\"_blank\" title=\"\" rel=\"noopener\">tardkivimid ehk magmakivimid<\/a>\n\t\t<\/p>\n<\/li>\n<li>\n<p>\n\t\t\t<a data-url=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/moondekivimid\" href=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/moondekivimid\" target=\"_blank\" title=\"\" rel=\"noopener\">moondekivimid ehk metamorfsed kivimid<\/a>\n\t\t<\/p>\n<\/li>\n<li>\n<p>\n\t\t\t<a data-url=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/settekivimid\" href=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/settekivimid\" target=\"_blank\" title=\"\" rel=\"noopener\">settekivimid<\/a>\n\t\t<\/p>\n<\/li>\n<\/ul>\n<p>\n\tK\u00f5igi kolme suure r\u00fchma kivimid erinevad nii keemilise koostise, koostismineraalide suhte kui ka ehituse poolest. Samal ajal on nad omavahel keerukalt seotud\u00a0(<a data-url=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/ringkaik\" href=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/ringkaik\" target=\"_blank\" title=\"\" rel=\"noopener\">skeem 1, 2<\/a>).\n<\/p>\n<p>\n\tTardkivimid ja moondel tekkinud kivimid moodustavad maakoore mahust 95%, kuid paljanduvad vaid 25%-l maismaa pindalast.\u00a0<a data-url=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/sete\" href=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/sete\" target=\"_blank\" title=\"\" rel=\"noopener\">Setted<\/a>\u00a0ja\u00a0<a data-url=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/settekivimid\" href=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/settekivimid\" target=\"_blank\" title=\"\" rel=\"noopener\">settekivimid<\/a>\u00a0moodustavad vaid 5% maakoore mahust, kuid katavad ligikaudu 75% maismaast.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tekkest l\u00e4htudes\u00a0eristatakse kolme kivimite suurt r\u00fchma (skeem 1 ja 2): \u00a0 tardkivimid ehk magmakivimid moondekivimid ehk metamorfsed kivimid settekivimid K\u00f5igi kolme suure r\u00fchma kivimid erinevad nii keemilise koostise, koostismineraalide suhte kui ka ehituse poolest. Samal ajal on nad omavahel keerukalt &#8230;<\/p>\n","protected":false},"author":226,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"inline_featured_image":false,"footnotes":""},"class_list":["post-132","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/pages\/132","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/users\/226"}],"replies":[{"embeddable":true,"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/comments?post=132"}],"version-history":[{"count":1,"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/pages\/132\/revisions"}],"predecessor-version":[{"id":715,"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/pages\/132\/revisions\/715"}],"wp:attachment":[{"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/media?parent=132"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}