{"id":473,"date":"2025-11-02T00:13:03","date_gmt":"2025-11-01T19:13:03","guid":{"rendered":"http:\/\/npzaamin.uz\/?page_id=473"},"modified":"2025-11-05T13:55:55","modified_gmt":"2025-11-05T08:55:55","slug":"geologiya","status":"publish","type":"page","link":"https:\/\/npzaamin.uz\/en\/tabiat\/geologiya\/","title":{"rendered":"Geology"},"content":{"rendered":"<p><\/p>\n<p class=\"p1\"><span class=\"s1\">The <\/span><b>geological structure<\/b><span class=\"s1\"> of the Zomin National Nature Park gives it a unique <\/span><b>character and coloration<\/b><span class=\"s1\">, significantly influencing the <\/span><b>formation of geomorphological and forest landscapes<\/b><span class=\"s1\">.<\/span><\/p>\n<p class=\"p3\">According to studies conducted by researchers of the <span class=\"s2\"><b>Tashkent State University<\/b><\/span>, the following <span class=\"s2\"><b>geomorphological landscape types<\/b><\/span> have been identified and examined:<\/p>\n<ul>\n<li>\n<p class=\"p1\"><b>Moist, high-mountain nivation forms of relief<\/b><span class=\"s1\">, located at <\/span><b>3700\u20134000 m<\/b><span class=\"s1\"> above sea level;<\/span><\/p>\n<\/li>\n<li>\n<p class=\"p1\"><span class=\"s1\"><b>Erosional-denudational high mountains<\/b><\/span>, dissected by steep cliffs and deep gorges, located at <span class=\"s1\"><b>3000\u20133700 m<\/b><\/span>;<\/p>\n<\/li>\n<li>\n<p class=\"p1\"><b>Paleozoic-era pre-Paleogene denudational coal formations<\/b><span class=\"s1\">, found at <\/span><b>around 3500 m<\/b><span class=\"s1\">;<\/span><\/p>\n<\/li>\n<li>\n<p class=\"p1\"><b>Erosional-accumulative highlands<\/b><span class=\"s1\"> with semi-steep slopes, <\/span><b>2100\u20132750 m<\/b><span class=\"s1\">;<\/span><\/p>\n<\/li>\n<li>\n<p class=\"p1\"><b>Mid-mountain pre-Paleogene denudational layers<\/b><span class=\"s1\">, formed during the Paleozoic era, <\/span><b>2200\u20133000 m<\/b><span class=\"s1\">;<\/span><\/p>\n<\/li>\n<li>\n<p class=\"p1\"><b>Accumulative-erosional terraced mid-mountains<\/b><span class=\"s1\">, <\/span><b>1650\u20132500 m<\/b><span class=\"s1\">;<\/span><\/p>\n<\/li>\n<li>\n<p class=\"p1\"><b>Canyon-shaped valleys<\/b><span class=\"s1\"> and <\/span><b>erosional-gravitational landforms<\/b><span class=\"s1\">, <\/span><b>1650\u20132160 m<\/b><span class=\"s1\">;<\/span><\/p>\n<\/li>\n<li>\n<p class=\"p1\"><b>Low-mountain accumulative-erosional foothills<\/b><span class=\"s1\">, <\/span><b>1200\u20132500 m<\/b><span class=\"s1\"> above sea level.<\/span><\/p>\n<\/li>\n<\/ul>\n<p class=\"p3\">These geomorphological features demonstrate that, despite their diversity, the <span class=\"s2\"><b>high-mountain regions<\/b><\/span> play a decisive role in the <span class=\"s2\"><b>differentiation of natural conditions<\/b><\/span>.<\/p>\n<p class=\"p3\">In the <span class=\"s2\"><b>northern part of the park<\/b><\/span> (particularly along the Yettikechuv, Urikli, and Usmonli streams), the geological structure consists mainly of <span class=\"s2\"><b>rocky slopes<\/b><\/span>.<\/p>\n<p class=\"p3\"><span class=\"s2\"><b>Paleozoic coal deposits<\/b><\/span> played a crucial role in the formation of the famous <span class=\"s2\"><b>Supa<\/b><\/span> and <span class=\"s2\"><b>Chortangi<\/b><\/span> depressions.<\/p>\n<p class=\"p3\">These distinctive geological features make the area highly attractive for <span class=\"s2\"><b>tourists and alpinists<\/b><\/span> alike.<\/p>\n<p><\/p>","protected":false},"excerpt":{"rendered":"<p>The geological structure of the Zomin National Nature Park gives it a unique character and coloration, significantly influencing the formation of geomorphological and forest landscapes. According to studies conducted by researchers of the Tashkent State University, the following geomorphological landscape types have been identified and examined: Moist, high-mountain nivation forms of relief, located at 3700\u20134000 [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":465,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-473","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/pages\/473","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/comments?post=473"}],"version-history":[{"count":2,"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/pages\/473\/revisions"}],"predecessor-version":[{"id":620,"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/pages\/473\/revisions\/620"}],"up":[{"embeddable":true,"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/pages\/465"}],"wp:attachment":[{"href":"https:\/\/npzaamin.uz\/en\/wp-json\/wp\/v2\/media?parent=473"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}