{"id":56212,"date":"2023-03-31T07:34:23","date_gmt":"2023-03-31T04:34:23","guid":{"rendered":"https:\/\/milliycha.uz\/?p=56212"},"modified":"2023-03-31T07:34:25","modified_gmt":"2023-03-31T04:34:25","slug":"balandlik-mintaqalari-2","status":"publish","type":"post","link":"https:\/\/milliycha.uz\/kr\/balandlik-mintaqalari-2\/","title":{"rendered":"Balandlik mintaqalari"},"content":{"rendered":"\n<p><strong>Balandlik mintaqalari <\/strong>&#8211; toqqa ko`tarilgan sari tabiatning o`zgarib borishi, balandlik mintaqalari quyosh radiatsiyasining kuchayishi, havo harorati va bosimning kamayishi, suv bug`lari kondensatsiyasi sharoitining o`zgarishidan paydo bo`ladi. Yog`in ma\u2019lum balandlikkacha ko`payib, so`ng kamayadi. Yuqoriga ko`tarilgan sari, tuproq tiplari, o`simlik turlari, hayvonot dunyosi o`zgaradi. Tog`lardagi eng quyi mintaqa landshaft &#8211; shu tog` joylashgan zona landshaftiga o`xshaydi. Masalan, cho`ldagi tog`larning quyi mintaqasi cho`lga o`xshaydi. Balandlik mintaqalari yuqoriga ko`tarilgan sari tekislik zonalari tabiati almashingan tartibda o`zgara boradi, biroq ular aynan takrorlanmaydi. O`rta Osiyo tog`larining tagida cho`l mintaqasi, so`ngra tog` dashtlari, undan keyin tog` o`rmonlari, undan tepada tog` o`tloqlari, yana ham yuqorida baland tog` cho`llari va nihoyat, qop-muz mintaqalari joylashgan.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Balandlik mintaqalari &#8211; toqqa ko`tarilgan sari tabiatning o`zgarib borishi, balandlik mintaqalari quyosh radiatsiyasining kuchayishi, havo harorati va bosimning kamayishi, suv bug`lari kondensatsiyasi sharoitining o`zgarishidan paydo bo`ladi. Yog`in ma\u2019lum balandlikkacha ko`payib, &hellip; <a href=\"https:\/\/milliycha.uz\/kr\/balandlik-mintaqalari-2\/\" class=\"more-link\">Read More<\/a><\/p>\n","protected":false},"author":1,"featured_media":55935,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[259],"tags":[],"class_list":["post-56212","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-b-harfiga-oid-geografiyaga-oid-ensiklopedik-atamalar","entry"],"translation":{"provider":"WPGlobus","version":"3.0.0","language":"kr","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\/kr\/wp-json\/wp\/v2\/posts\/56212","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/comments?post=56212"}],"version-history":[{"count":1,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/posts\/56212\/revisions"}],"predecessor-version":[{"id":56225,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/posts\/56212\/revisions\/56225"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/media\/55935"}],"wp:attachment":[{"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/media?parent=56212"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/categories?post=56212"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/tags?post=56212"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}