{"id":8992,"date":"2024-06-24T09:57:38","date_gmt":"2024-06-23T23:57:38","guid":{"rendered":"https:\/\/scienceillustrated.com.au\/blog\/?p=8992"},"modified":"2024-06-24T09:57:38","modified_gmt":"2024-06-23T23:57:38","slug":"why-is-the-worlds-largest-volcano-in-the-middle-of-nowhere","status":"publish","type":"post","link":"https:\/\/scienceillustrated.com.au\/blog\/features\/why-is-the-worlds-largest-volcano-in-the-middle-of-nowhere\/","title":{"rendered":"Why is the world&#8217;s largest volcano in the middle of nowhere?"},"content":{"rendered":"<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-8993\" src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/uploads\/2024\/06\/hawaii.jpg\" alt=\"Wirestock Creators\/Shutterstock\" width=\"1920\" height=\"1080\" srcset=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/uploads\/2024\/06\/hawaii.jpg 1920w, https:\/\/scienceillustrated.com.au\/blog\/wp-content\/uploads\/2024\/06\/hawaii-300x169.jpg 300w, https:\/\/scienceillustrated.com.au\/blog\/wp-content\/uploads\/2024\/06\/hawaii-1024x576.jpg 1024w, https:\/\/scienceillustrated.com.au\/blog\/wp-content\/uploads\/2024\/06\/hawaii-768x432.jpg 768w, https:\/\/scienceillustrated.com.au\/blog\/wp-content\/uploads\/2024\/06\/hawaii-1536x864.jpg 1536w, https:\/\/scienceillustrated.com.au\/blog\/wp-content\/uploads\/2024\/06\/hawaii-460x260.jpg 460w\" sizes=\"(max-width: 1920px) 100vw, 1920px\" \/><\/p>\n<p class=\"p1\"><strong>Mauna Loa in Hawaii is the world\u2019s largest active volcano, and its 2022 eruption was the volcano\u2019s 34th since 1843. But why is such a giant volcano located in the middle of the Pacific Ocean, far away from everything?<\/strong><\/p>\n<p class=\"p1\">In a nutshell, this area is the place on Earth where the most magma per square kilometre reaches Earth\u2019s surface. All of the Hawaiian Islands \u2013 eight major islands and many smaller ones \u2013 were formed by volcanoes.<\/p>\n<p class=\"p2\">Mauna Loa measures 17km from its base under the ocean to the ridge of the crater at its summit. Like the other Hawaiian volcanoes, Mauna Loa was formed due to what geologists call a hotspot \u2014 an area under Earth&#8217;s crust where a lot of magma is formed. As a result, extra large volcanoes form above the hotspots.<\/p>\n<p class=\"p2\">The Hawaiian volcanoes are shield volcanoes \u2013 wide and relatively flat volcanoes made up of basaltic magma. Nearly<span class=\"Apple-converted-space\">\u00a0 <\/span>all the ocean floor is made up of basaltic magma, which flows far and easily at speeds of up to 16km\/h. This results in volcanoes that look like a knight&#8217;s shield facing upwards. There is little slope on the sides of the volcano, so a tall shield volcano can covers a huge area. The largest island, Hawaii, or the Big Island, was formed by five overlapping shield volcanoes; it covers an area of around 10,430km\u00b2.<\/p>\n<p class=\"p2\">Observed from above, the Hawaiian Islands are located on a line. This is because the hotspot is constantly forming new volcanoes south-east of the old ones. However, it is not the hotspot that is moving \u2014 rather it is the Pacific tectonic plate that is moving to the north-west, while the hotspot sits below Earth\u2019s crust at a standstill.<\/p>\n<p class=\"p2\">In 1971, this led geophysicist Jason W. Morgan to introduce a revolutionary theory about mantle plumes. A mantle plume is a bubble of particularly hot material that rises up from Earth\u2019s core in a particular place. As well as the one that is probably located under Hawaii, geologists believe that the Yellowstone supervolcano in the US is also atop a mantle plume which is \u2018moving\u2019 under its plate.<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-8994\" src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/uploads\/2024\/06\/mantle.jpg\" alt=\"Shutterstock\/SI\" width=\"1787\" height=\"626\" srcset=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/uploads\/2024\/06\/mantle.jpg 1787w, https:\/\/scienceillustrated.com.au\/blog\/wp-content\/uploads\/2024\/06\/mantle-300x105.jpg 300w, https:\/\/scienceillustrated.com.au\/blog\/wp-content\/uploads\/2024\/06\/mantle-1024x359.jpg 1024w, https:\/\/scienceillustrated.com.au\/blog\/wp-content\/uploads\/2024\/06\/mantle-768x269.jpg 768w, https:\/\/scienceillustrated.com.au\/blog\/wp-content\/uploads\/2024\/06\/mantle-1536x538.jpg 1536w\" sizes=\"(max-width: 1787px) 100vw, 1787px\" \/><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Mauna Loa in Hawaii is the world\u2019s largest active volcano, and its 2022 eruption was the volcano\u2019s 34th since 1843. But why is such a giant volcano located in the middle of the&#8230;<\/p>\n","protected":false},"author":15,"featured_media":8993,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[52,4,37],"tags":[982,983,321],"class_list":["post-8992","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-ask-us","category-features","category-geology","tag-hawaii","tag-mauna-loa","tag-volcano"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/posts\/8992"}],"collection":[{"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/users\/15"}],"replies":[{"embeddable":true,"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/comments?post=8992"}],"version-history":[{"count":1,"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/posts\/8992\/revisions"}],"predecessor-version":[{"id":8995,"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/posts\/8992\/revisions\/8995"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/media\/8993"}],"wp:attachment":[{"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/media?parent=8992"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/categories?post=8992"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/tags?post=8992"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}