{"id":86955,"date":"2026-02-09T17:36:34","date_gmt":"2026-02-09T12:06:34","guid":{"rendered":"https:\/\/vajiramandravi.com\/current-affairs\/?p=86955"},"modified":"2026-02-09T17:36:34","modified_gmt":"2026-02-09T12:06:34","slug":"karakoram-range","status":"publish","type":"post","link":"https:\/\/vajiramandravi.com\/current-affairs\/karakoram-range\/","title":{"rendered":"Karakoram Range, Location, Physiography, Drainage, Ecology"},"content":{"rendered":"<p><span style=\"font-weight: 400;\">The Karakoram Range, also known as <\/span><b>Krishnagiri<\/b><span style=\"font-weight: 400;\">, is the northernmost <\/span><b>Trans-Himalayan range<\/b><span style=\"font-weight: 400;\"> in India. The name Karakoram is derived from a Turkic term meaning <\/span><b>\u201cBlack Rock\u201d or \u201cBlack Mountain.\u201d<\/b><\/p>\n<p><span style=\"font-weight: 400;\">The range is geopolitically significant as the borders of India, Pakistan, China, Afghanistan, and Tajikistan converge in this region.<\/span><\/p>\n<h2><b>Karakoram Range Location and Extent<\/b><\/h2>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The Karakoram range is a mountain range in <\/span><b>Asia<\/b><span style=\"font-weight: 400;\"> located primarily in the <\/span><b>Kashmir region.<\/b><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">It lies to the <\/span><b>north of the Great Himalayan Range<\/b><span style=\"font-weight: 400;\"> and extends across <\/span><b>Ladakh in India, Gilgit-Baltistan in Pakistan, and Xinjiang in China.<\/b><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">It is a part of the <\/span><b>Trans-Himalayan mountain system.\u00a0<\/b><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">It is bounded by Pamir Plateau in the northwest, Kunlun Mountains in the north, Himalayan Range in the south.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The range runs in a <\/span><b>north-west to south-east direction<\/b><span style=\"font-weight: 400;\"> and acts as a natural barrier between the Indian subcontinent and Central Asia.<\/span><\/li>\n<\/ul>\n<h2><b>Karakoram Range Geology<\/b><\/h2>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The Karakoram range was formed during the <\/span><b>Cenozoic era.<\/b><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">It is a <\/span><b>young fold mountain range<\/b><span style=\"font-weight: 400;\">. It formed due to the collision of the <\/span><b>Indian Plate with the Eurasian Plate.<\/b><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Due to active tectonics, the region is <\/span><b>highly prone to <a href=\"https:\/\/vajiramandravi.com\/upsc-exam\/earthquake\/\" target=\"_blank\">earthquakes<\/a> and <a href=\"https:\/\/vajiramandravi.com\/upsc-exam\/landslides\/\" target=\"_blank\">landslides<\/a>.<\/b><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The region is structurally complex and consists mainly of <\/span><b>igneous and metamorphic rocks, such as granite and gneiss.<\/b><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Major geological features include the <\/span><b>Karakoram Fault <\/b><span style=\"font-weight: 400;\">and the <\/span><b>Indus-Tsangpo Suture Zone<\/b><span style=\"font-weight: 400;\">, which indicate intense tectonic activity.<\/span><\/li>\n<\/ul>\n<h2><b>Karakoram Range Relief and Physiography<\/b><\/h2>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The Karakoram Range is known for its <\/span><b>extremely rugged and steep terrain<\/b><span style=\"font-weight: 400;\">.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The Karakoram Range contains some of the highest peaks on Earth including <\/span><b>K2 (Mount Godwin-Austen)<\/b><span style=\"font-weight: 400;\">, at 8,611 metres, which is the <\/span><b>second highest peak in the world.<\/b><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The Karakoram Range is marked by <\/span><b>deep, narrow, and glaciated valleys<\/b><span style=\"font-weight: 400;\"> formed by tectonic uplift and intense glacial erosion. Important valleys include the <\/span><b>Nubra Valley in Ladakh, Hunza Valley in Gilgit-Baltistan, Shigar Valley, Shimshal Valley.\u00a0<\/b><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The Karakoram Range contains several high-altitude passes such as the <\/span><b>Karakoram Pass, Khunjerab Pass, and Saser La, <\/b><span style=\"font-weight: 400;\">which have historically served as trade and strategic routes between South Asia, Central Asia, and China.<\/span><\/li>\n<\/ul>\n<h2><b>Karakoram Range Glaciers<\/b><\/h2>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The Karakoram Range is one of the <\/span><b>most heavily glaciated regions <\/b><span style=\"font-weight: 400;\">outside the polar areas.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Major glaciers include the <\/span><b>Siachen Glacier, Baltoro Glacier, Biafo Glacier, and Hispar Glacier.<\/b><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The region exhibits the <\/span><b>Karakoram Anomaly<\/b><span style=\"font-weight: 400;\">, where many glaciers are stable or advancing despite global warming trends. This anomaly is attributed to high-altitude snowfall, lower summer temperatures, and the dominance of western disturbances.<\/span><\/li>\n<\/ul>\n<h2><b>Karakoram Range Drainage<\/b><\/h2>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The rivers of the Karakoram Range are mainly glacier-fed.\u00a0<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The Karakoram Range acts as a <\/span><b>water divide<\/b><span style=\"font-weight: 400;\">, with rivers on its southern side draining into the <\/span><b>Indus basin<\/b><span style=\"font-weight: 400;\"> and those on the northern side draining into the <\/span><b>Yarkand &#8211; Tarim basin.<\/b><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Rivers such as the <\/span><b>Indus, Shyok, Nubra, and Hunza <\/b><span style=\"font-weight: 400;\">originate from or are fed by Karakoram glaciers.<\/span><\/li>\n<\/ul>\n<h2><b>Karakoram Range Climate\u00a0<\/b><\/h2>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Karakoram Range experiences a cold desert climate with extremely low annual precipitation.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The Indian monsoon has very little influence on the region, and most precipitation occurs in the form of winter snowfall due to western disturbances.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The region experiences long, severe winters and short, cool summers, along with large diurnal temperature variations.<\/span><\/li>\n<\/ul>\n<h2><b>Karakoram Range Ecology and Biodiversity<\/b><\/h2>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Due to harsh climatic conditions, vegetation in the Karakoram is sparse and mainly consists of alpine grasses and cold desert shrubs.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Despite extreme conditions, the region supports rare wildlife such as the <\/span><b>snow leopard, Himalayan ibex, and blue sheep.<\/b><\/li>\n<\/ul>\n","protected":false},"excerpt":{"rendered":"<p>Karakoram Range is the northernmost Trans-Himalayan range covering Ladakh, Pakistan and China, known for K2, major glaciers, unique drainage and ecology.<\/p>\n","protected":false},"author":11,"featured_media":86992,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[786],"tags":[4935,5102,5276],"class_list":{"0":"post-86955","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","7":"category-general-studies","8":"tag-geography","9":"tag-geography-notes","10":"tag-karakoram-range","11":"no-featured-image-padding"},"acf":[],"_links":{"self":[{"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/posts\/86955","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/users\/11"}],"replies":[{"embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/comments?post=86955"}],"version-history":[{"count":3,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/posts\/86955\/revisions"}],"predecessor-version":[{"id":86970,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/posts\/86955\/revisions\/86970"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/media\/86992"}],"wp:attachment":[{"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/media?parent=86955"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/categories?post=86955"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/tags?post=86955"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}