{"id":76,"date":"2019-08-15T21:00:47","date_gmt":"2019-08-16T01:00:47","guid":{"rendered":"http:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/?p=76"},"modified":"2020-05-01T12:57:15","modified_gmt":"2020-05-01T16:57:15","slug":"far-far-away-behind-the-word-mountains","status":"publish","type":"post","link":"https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/far-far-away-behind-the-word-mountains\/","title":{"rendered":"Far far away, behind the word mountains"},"content":{"rendered":"\n<p>A mountain is a large landform that rises above the surrounding land in a limited area, usually in the form of a peak. A mountain is generally steeper than a hill. <strong>Mountains <\/strong>are formed through tectonic forces or volcanism. <\/p>\n\n\n\n<p>These forces can locally raise the surface of the earth. Mountains erode slowly through the action of rivers, <a href=\"#\">weather conditions<\/a>, and glaciers. A few mountains are isolated summits, but most occur in huge <strong>mountain ranges<\/strong>.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"683\" src=\"https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/themes\/veen\/assets\/images\/transparent.gif\" data-lazy=\"true\" data-src=\"http:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/08\/chris-lawton-c0rIh0nFTFU-unsplash-1024x683.jpg\" alt=\"\" class=\"wp-image-414\" data-srcset=\"https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/08\/chris-lawton-c0rIh0nFTFU-unsplash-1024x683.jpg 1024w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/08\/chris-lawton-c0rIh0nFTFU-unsplash-300x200.jpg 300w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/08\/chris-lawton-c0rIh0nFTFU-unsplash-768x512.jpg 768w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/08\/chris-lawton-c0rIh0nFTFU-unsplash-1536x1024.jpg 1536w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/08\/chris-lawton-c0rIh0nFTFU-unsplash-100x67.jpg 100w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/08\/chris-lawton-c0rIh0nFTFU-unsplash-675x450.jpg 675w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/08\/chris-lawton-c0rIh0nFTFU-unsplash.jpg 1600w\" data-sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<p>High elevations on mountains produce colder climates than at sea level. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains tend to be used <strong>less for agriculture<\/strong> and more for resource extraction and recreation, such as mountain climbing.<\/p>\n\n\n\n<p>The highest mountain on <strong>Earth <\/strong>is <strong>Mount Everest<\/strong> in the <strong>Himalayas of Asia<\/strong>, whose summit is 8,850 m (29,035 ft) above mean sea level. The highest known mountain on any planet in the <a href=\"#\">Solar System<\/a> is Olympus Mons on Mars at 21,171 m (69,459 ft).<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Definition<\/h2>\n\n\n\n<p>There is no universally accepted definition of a mountain. Elevation, volume, relief, steepness, spacing and continuity have been used as criteria for defining a mountain. In the <strong>Oxford English Dictionary<\/strong> a mountain is defined as &#8220;a natural elevation of the earth surface rising more or less abruptly from the surrounding level and attaining an altitude which, relatively to the adjacent elevation, is impressive or notable.&#8221;<\/p>\n\n\n\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"597\" src=\"https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/themes\/veen\/assets\/images\/transparent.gif\" data-lazy=\"true\" data-src=\"http:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/alex-cKH9F7Wjn9U-unsplash-1024x597.jpg\" alt=\"\" class=\"wp-image-498\" data-srcset=\"https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/alex-cKH9F7Wjn9U-unsplash-1024x597.jpg 1024w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/alex-cKH9F7Wjn9U-unsplash-300x175.jpg 300w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/alex-cKH9F7Wjn9U-unsplash-768x448.jpg 768w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/alex-cKH9F7Wjn9U-unsplash-1536x896.jpg 1536w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/alex-cKH9F7Wjn9U-unsplash-100x58.jpg 100w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/alex-cKH9F7Wjn9U-unsplash-700x408.jpg 700w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/alex-cKH9F7Wjn9U-unsplash.jpg 1600w\" data-sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><figcaption>Pink paper over blue background<\/figcaption><\/figure><\/div>\n\n\n\n<p>Whether a landform is called a mountain may depend on local usage. Mount Scott outside Lawton, <strong>Oklahoma, USA<\/strong>, is only 251 m (823 ft) from its base to its highest point. <\/p>\n\n\n\n<blockquote class=\"wp-block-quote is-layout-flow wp-block-quote-is-layout-flow\"><p>Physical Geography states &#8220;Some authorities regard eminences above 600 metres (2,000 ft) as mountains, those below being referred to as hills.&#8221;<\/p><cite> Whittow&#8217;s Dictionary <\/cite><\/blockquote>\n\n\n\n<h2 class=\"wp-block-heading\">Geology<\/h2>\n\n\n\n<p>There are <strong>three main types of mountains<\/strong>:&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Volcano\">volcanic<\/a>,&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Fold_mountain\">fold<\/a>, and&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Fault-block_mountain\">block<\/a>.&nbsp;All three types are formed from&nbsp;plate tectonics: when portions of the Earth&#8217;s crust <strong>move<\/strong>, <strong>crumple<\/strong>, and <strong>dive<\/strong>. Compressional forces,&nbsp;isostatic&nbsp;uplift&nbsp;and intrusion of&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Igneous_rock\">igneous matter<\/a>&nbsp;forces surface rock upward, creating a landform higher than the surrounding features. The height of the feature makes it either a hill or, if higher and steeper, a mountain. Major mountains tend to occur in <strong>long linear arcs<\/strong>, indicating tectonic plate boundaries and activity. <\/p>\n\n\n\n<h3 class=\"wp-block-heading\">Volcanoes<\/h3>\n\n\n\n<p><strong>Volcanoes <\/strong>are formed when&nbsp;a plate is <strong>pushed below another plate<\/strong>, or at a&nbsp;mid-ocean ridge&nbsp;or&nbsp;hotspot.&nbsp;At a depth of around 100&nbsp;km, melting occurs in rock above the slab (due to the addition of water), and forms&nbsp;magma&nbsp;that reaches the surface. When the magma reaches the surface, it often builds a volcanic mountain, such as a&nbsp;shield volcano&nbsp;or a&nbsp;stratovolcano.&nbsp;<strong>Examples of volcanoes<\/strong> include&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Mount_Fuji\">Mount Fuji<\/a>&nbsp;in Japan and&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Mount_Pinatubo\">Mount Pinatubo<\/a>&nbsp;in the Philippines. The magma does not have to reach the surface in order to create a mountain: magma that solidifies below ground can still form&nbsp;dome mountains, such as&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Navajo_Mountain\">Navajo Mountain<\/a>&nbsp;in the US. <\/p>\n\n\n\n<h3 class=\"wp-block-heading\">Fold mountains<\/h3>\n\n\n\n<p><strong>Fold mountains<\/strong> occur when two plates collide: shortening occurs along thrust faults and the crust is overthickened.&nbsp;Since the less dense&nbsp;continental crust&nbsp;&#8220;floats&#8221; on the denser&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Mantle_(geology)\">mantle<\/a>&nbsp;rocks beneath, the weight of any crustal material forced upward to form hills,&nbsp;plateaus&nbsp;or mountains must be&nbsp;balanced by the buoyancy force&nbsp;of a much greater volume forced downward into the mantle. Thus the continental crust is normally much thicker under mountains, compared to lower lying areas.&nbsp;Rock can&nbsp;fold&nbsp;either <strong>symmetrically <\/strong>or <strong>asymmetrically<\/strong>. The upfolds are&nbsp;anticlines&nbsp;and the downfolds are&nbsp;synclines: in asymmetric folding there may also be recumbent and overturned folds. The&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Balkan_Mountains\">Balkan Mountains<\/a>&nbsp;and the&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Jura_Mountains\">Jura Mountains<\/a>&nbsp;are examples of fold mountains. <\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"602\" src=\"https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/themes\/veen\/assets\/images\/transparent.gif\" data-lazy=\"true\" data-src=\"http:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/gareth-harper-yACpBcInUos-unsplash-1024x602.jpg\" alt=\"\" class=\"wp-image-441\" data-srcset=\"https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/gareth-harper-yACpBcInUos-unsplash-1024x602.jpg 1024w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/gareth-harper-yACpBcInUos-unsplash-300x176.jpg 300w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/gareth-harper-yACpBcInUos-unsplash-768x451.jpg 768w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/gareth-harper-yACpBcInUos-unsplash-1536x902.jpg 1536w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/gareth-harper-yACpBcInUos-unsplash-100x59.jpg 100w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/gareth-harper-yACpBcInUos-unsplash-700x411.jpg 700w, https:\/\/estudiopatagon.com\/themes\/wordpress\/veenv2\/wp-content\/uploads\/2019\/07\/gareth-harper-yACpBcInUos-unsplash.jpg 1600w\" data-sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><figcaption>This is a example caption<\/figcaption><\/figure>\n\n\n\n<h3 class=\"wp-block-heading\">Block mountains<\/h3>\n\n\n\n<p>B<strong>lock mountains<\/strong> are caused by&nbsp;faults&nbsp;in the crust: a plane where rocks have moved past each other. When rocks on one side of a fault rise relative to the other, it can form a mountain.&nbsp;The uplifted blocks are <strong>block mountains<\/strong> or&nbsp;<strong>horsts<\/strong>. The intervening dropped blocks are termed&nbsp;graben: these can be small or form extensive&nbsp;rift valley&nbsp;systems. This form of&nbsp;landscape&nbsp;can be seen in&nbsp;East Africa, the&nbsp;Vosges, the&nbsp;Basin and Range Province&nbsp;of <strong>Western North America<\/strong> and the&nbsp;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Rhine_graben\">Rhine<\/a>&nbsp;valley. These areas often occur when the regional stress is extensional and the&nbsp;crust&nbsp;is thinned. <\/p>\n","protected":false},"excerpt":{"rendered":"<p>A mountain is a large landform that rises above the surrounding land in a limited area, usually in the form of a peak. A mountain&#8230;<\/p>\n","protected":false},"author":2,"featured_media":416,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[5],"tags":[15],"class_list":["post-76","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-travel","tag-definitions"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.2 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Far far away, behind the word mountains - Veen<\/title>\n<meta name=\"description\" content=\"A mountain is a large landform that rises above the surrounding land in a limited area, usually in the form of a peak. 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