{"id":124852,"date":"2024-05-18T20:16:08","date_gmt":"2024-05-18T17:16:08","guid":{"rendered":"https:\/\/milliycha.uz\/?p=124852"},"modified":"2024-05-18T20:16:11","modified_gmt":"2024-05-18T17:16:11","slug":"suv-osti-vodiylari-2","status":"publish","type":"post","link":"https:\/\/milliycha.uz\/ru\/suv-osti-vodiylari-2\/","title":{"rendered":"Suv osti vodiylari"},"content":{"rendered":"\n<p>Suv osti vodiylari, suv osti kan&#8217;onlari \u2014 dengiz va okeanlar tubi- ning erozion, tektonik kuchlar ta&#8217;siri- da o&#8217;yilishi natijasida hosil bo&#8217;lgan uzun cho&#8217;zilgan to&#8217;g&#8217;ri yoki egribugri chuqurliklar. Dengiz va okeanlarning materik sayozligi, yon bag&#8217;ri va tubida uch- raydi. Erozion So.v. daryolarning den- gizga quyilish qismining cho&#8217;kishi yoki dengiz sathining ko&#8217;tarilishi oqibatida hamda quruqlikdan keltirilgan turli mayda jinslarga boy dengiz osti Su- spenzion oqimlarning ishi natijasida xreil bo&#8217;ladi. Ba&#8217;zi S.o.v. yirik daryolar quyilish erining davomi hisoblanadi. Dengiz sathining ko&#8217;tarilishi nati- jasida daryolarning suv ostida qolib ketgan vodiylari yaxshi saqlangan (Gud- zon, Hind, Kongo va b.). Materik yon bag&#8217;irlarida bunday vodiylar V Simon shakldagi jo&#8217;yaklarni, Nishab akkumu- lyativ shleyflar va okean tubi tekis- liklarida chuq. 50 m dan bir necha yuz m gacha, eni 1-3 km, uz. 100 hatto ming km ga cho&#8217;zilgan egribugri vodiylarni Vu- judga keltiradi. Tektonik S.o.v. ocean o&#8217;rtaliq suv osti tizmalari zonalari- ning Markaziy (Rift) qismida materik chetlarining yorilishi, sinishidan yuzaga keladi. S.o.v.ning kelib chiqishida muz- liklar ham bevosita rol o&#8217;ynaydi.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Suv osti vodiylari, suv osti kan&#8217;onlari \u2014 dengiz va okeanlar tubi- ning erozion, tektonik kuchlar ta&#8217;siri- da o&#8217;yilishi natijasida hosil bo&#8217;lgan uzun cho&#8217;zilgan to&#8217;g&#8217;ri yoki egribugri chuqurliklar. Dengiz va okeanlarning &hellip; <a href=\"https:\/\/milliycha.uz\/ru\/suv-osti-vodiylari-2\/\" class=\"more-link\">Read More<\/a><\/p>\n","protected":false},"author":1,"featured_media":99837,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[206],"tags":[],"class_list":["post-124852","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-s-harfi","entry"],"translation":{"provider":"WPGlobus","version":"3.0.2","language":"ru","enabled_languages":["uz","kr","ru"],"languages":{"uz":{"title":true,"content":true,"excerpt":false},"kr":{"title":false,"content":false,"excerpt":false},"ru":{"title":false,"content":false,"excerpt":false}}},"_links":{"self":[{"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/posts\/124852","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/comments?post=124852"}],"version-history":[{"count":1,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/posts\/124852\/revisions"}],"predecessor-version":[{"id":124864,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/posts\/124852\/revisions\/124864"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/media\/99837"}],"wp:attachment":[{"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/media?parent=124852"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/categories?post=124852"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/tags?post=124852"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}