{"id":140,"date":"2024-12-02T09:05:16","date_gmt":"2024-12-02T09:05:16","guid":{"rendered":"http:\/\/62.72.56.4:2020\/?p=140"},"modified":"2024-12-08T06:38:32","modified_gmt":"2024-12-08T06:38:32","slug":"mountain","status":"publish","type":"post","link":"https:\/\/kul.af\/index.php\/2024\/12\/02\/mountain\/","title":{"rendered":"Mountain"},"content":{"rendered":"\n<figure class=\"wp-block-image size-large is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"682\" src=\"http:\/\/62.72.56.4\/wp-content\/uploads\/2024\/12\/Everest_North_Face_toward_Base_Camp_Tibet_Luca_Galuzzi_2006-1024x682.jpg\" alt=\"\" class=\"wp-image-141\" style=\"width:1200px;height:auto\" srcset=\"https:\/\/kul.af\/wp-content\/uploads\/2024\/12\/Everest_North_Face_toward_Base_Camp_Tibet_Luca_Galuzzi_2006-1024x682.jpg 1024w, https:\/\/kul.af\/wp-content\/uploads\/2024\/12\/Everest_North_Face_toward_Base_Camp_Tibet_Luca_Galuzzi_2006-300x200.jpg 300w, https:\/\/kul.af\/wp-content\/uploads\/2024\/12\/Everest_North_Face_toward_Base_Camp_Tibet_Luca_Galuzzi_2006-768x512.jpg 768w, https:\/\/kul.af\/wp-content\/uploads\/2024\/12\/Everest_North_Face_toward_Base_Camp_Tibet_Luca_Galuzzi_2006-1536x1024.jpg 1536w, https:\/\/kul.af\/wp-content\/uploads\/2024\/12\/Everest_North_Face_toward_Base_Camp_Tibet_Luca_Galuzzi_2006.jpg 2000w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<p>A&nbsp;<strong>mountain<\/strong>&nbsp;is an elevated portion of the&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Earth%27s_crust\">Earth&#8217;s crust<\/a>, generally with steep sides that show significant exposed&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Bedrock\">bedrock<\/a>. Although definitions vary, a mountain may differ from a&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Plateau\">plateau<\/a>&nbsp;in having a limited&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Summit\">summit<\/a>&nbsp;area, and is usually higher than a&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Hill\">hill<\/a>, typically rising at least 300&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Metre\">metres<\/a>&nbsp;(980&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Foot_(unit)\">ft<\/a>) above the surrounding land. A few mountains are&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Inselberg\">isolated summits<\/a>, but most occur in&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Mountain_range\">mountain ranges<\/a>.<sup><a href=\"https:\/\/en.wikipedia.org\/wiki\/Mountain#cite_note-agi-1997-1\">[1]<\/a><\/sup><\/p>\n\n\n\n<p><a href=\"https:\/\/en.wikipedia.org\/wiki\/Mountain_formation\">Mountains are formed<\/a>&nbsp;through&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Tectonic_plate\">tectonic forces<\/a>,&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Erosion\">erosion<\/a>, or&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Volcanism\">volcanism<\/a>,<sup><a href=\"https:\/\/en.wikipedia.org\/wiki\/Mountain#cite_note-agi-1997-1\">[1]<\/a><\/sup>&nbsp;which act on time scales of up to tens of millions of years.<sup><a href=\"https:\/\/en.wikipedia.org\/wiki\/Mountain#cite_note-levin-2010-83-2\">[2]<\/a><\/sup>&nbsp;Once mountain building ceases, mountains are slowly leveled through the action of&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Weathering\">weathering<\/a>, through&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Slump_(geology)\">slumping<\/a>&nbsp;and other forms of&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Mass_wasting\">mass wasting<\/a>, as well as through erosion by&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/River\">rivers<\/a>&nbsp;and&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Glacier\">glaciers<\/a>.<sup><a href=\"https:\/\/en.wikipedia.org\/wiki\/Mountain#cite_note-:0-3\">[3]<\/a><\/sup><\/p>\n\n\n\n<p>High elevations on mountains produce&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Alpine_climate\">colder climates<\/a>&nbsp;than at&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Sea_level\">sea level<\/a>&nbsp;at similar latitude. These colder climates strongly affect the&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Montane_ecosystems\">ecosystems<\/a>&nbsp;of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains tend to be used less for agriculture and more for resource extraction, such as&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Mining\">mining<\/a>&nbsp;and&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Logging\">logging<\/a>, along with recreation, such as&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Mountain_climbing\">mountain climbing<\/a>&nbsp;and&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Skiing\">skiing<\/a>.<\/p>\n\n\n\n<p>The highest mountain on Earth is&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Mount_Everest\">Mount Everest<\/a>&nbsp;in the&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Himalayas\">Himalayas<\/a>&nbsp;of&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Asia\">Asia<\/a>, whose summit is 8,850&nbsp;m (29,035&nbsp;ft) above mean sea level. The&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/List_of_tallest_mountains_in_the_Solar_System\">highest known mountain<\/a>&nbsp;on any planet in the Solar System is&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Olympus_Mons\">Olympus Mons<\/a>&nbsp;on Mars at 21,171&nbsp;m (69,459&nbsp;ft). The tallest mountain including submarine terrain is&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Mauna_Kea\">Mauna Kea<\/a>&nbsp;in&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Hawaii\">Hawaii<\/a>&nbsp;from its underwater base at 9,330 m (30,610 ft) and some scientists consider it to be the tallest on earth.<sup><a href=\"https:\/\/en.wikipedia.org\/wiki\/Mountain#cite_note-:0-3\">[3]<\/a><\/sup><\/p>\n","protected":false},"excerpt":{"rendered":"<p>A&nbsp;mountain&nbsp;is an elevated portion of the&nbsp;Earth&#8217;s crust, generally with steep sides that show significant exposed&nbsp;bedrock. Although definitions vary, a mountain may differ from a&nbsp;plateau&nbsp;in having a limited&nbsp;summit&nbsp;area, and is usually higher than a&nbsp;hill, typically rising at least 300&nbsp;metres&nbsp;(980&nbsp;ft) above the surrounding land. A few mountains are&nbsp;isolated summits, but most occur in&nbsp;mountain ranges.[1] Mountains are formed&nbsp;through&nbsp;tectonic [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":141,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[19],"tags":[],"class_list":["post-140","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-library-guide"],"_links":{"self":[{"href":"https:\/\/kul.af\/index.php\/wp-json\/wp\/v2\/posts\/140","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/kul.af\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/kul.af\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/kul.af\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/kul.af\/index.php\/wp-json\/wp\/v2\/comments?post=140"}],"version-history":[{"count":1,"href":"https:\/\/kul.af\/index.php\/wp-json\/wp\/v2\/posts\/140\/revisions"}],"predecessor-version":[{"id":142,"href":"https:\/\/kul.af\/index.php\/wp-json\/wp\/v2\/posts\/140\/revisions\/142"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/kul.af\/index.php\/wp-json\/wp\/v2\/media\/141"}],"wp:attachment":[{"href":"https:\/\/kul.af\/index.php\/wp-json\/wp\/v2\/media?parent=140"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/kul.af\/index.php\/wp-json\/wp\/v2\/categories?post=140"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/kul.af\/index.php\/wp-json\/wp\/v2\/tags?post=140"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}