{"id":90933,"date":"2023-01-22T18:24:00","date_gmt":"2023-01-22T22:24:00","guid":{"rendered":"https:\/\/www.shortform.com\/blog\/?p=90933"},"modified":"2023-01-31T12:34:02","modified_gmt":"2023-01-31T16:34:02","slug":"interior-parts-of-earth","status":"publish","type":"post","link":"https:\/\/www.shortform.com\/blog\/interior-parts-of-earth\/","title":{"rendered":"The Interior Parts of Earth: What&#8217;s Down Below the Surface?"},"content":{"rendered":"\n<p>How much do we know about the interior parts of Earth? What are the current theories?<\/p>\n\n\n\n<p>Contrary to what you&#8217;ll see in sci-fi movies, nobody&#8217;s been to the center of the Earth. We can dig only so deep. So, scientists have to resort to some indirect ways of determining what&#8217;s far below the Earth&#8217;s surface.<\/p>\n\n\n\n<p>Continue reading to learn what scientists believe and why.<\/p>\n\n\n\n<!--more-->\n\n\n\n<h2 class=\"wp-block-heading\" id=\"h-the-interior-parts-of-earth\">The Interior Parts of Earth<\/h2>\n\n\n\n<p>Bryson explains that, although the surface of planet Earth cooled and solidified billions of years ago, the interior of the planet is still hot enough to be molten. Scientists speculate that nuclear fission in the Earth\u2019s core may provide an ongoing source of heating, but we actually know relatively little about the interior parts of Earth because we can\u2019t directly observe them\u2014even the deepest mines and boreholes barely scratch the surface.<\/p>\n\n\n\n<p>(Shortform note: There is debate in the scientific community about how nuclear heating of the core would work. As Bryson recounts, some scientists have attributed it to the fission of heavy elements like uranium. But others point out that if you get enough uranium together in one place to start a fission chain reaction, the reaction tends to use up the nuclear fuel rather quickly. They argue that if uranium fission was the heating mechanism, Earth\u2019s core should have cooled off a long time ago. One alternative theory is that <a href=\"https:\/\/www.sciencedaily.com\/releases\/2003\/05\/030508080106.htm#:~:text=with%20its%20half-life%20of%201.3%20billion,the%20magnetic%20field%20for%20billions%20of\" target=\"_blank\" rel=\"noreferrer noopener\">the heat comes from the gradual radioactive decay of large quantities of potassium-40 in the core<\/a>. But scientists are divided on whether the core contains enough potassium for this to be possible.)<\/p>\n\n\n\n<p>So, scientists have to resort to indirect methods of probing the Earth&#8217;s interior. One source of information is the data recorded by seismographs, which record vibrations from Earthquakes. By comparing readings from seismographs in different locations, scientists can identify regions of different densities within the Earth.&nbsp;<\/p>\n\n\n\n<p>According to Bryson, scientists have deduced by this method that Earth has four distinct layers: The outer \u201ccrust\u201d is solid and just a few miles thick. The \u201cmantle\u201d comprises most of Earth\u2019s interior, and is essentially made of molten rock\u2014most of the rock isn\u2019t quite liquid but is hot enough to have a \u201cplastic\u201d consistency, somewhat like modeling clay. The \u201couter core\u201d appears to be liquid metal, while the \u201cinner core\u201d is solid and probably also metallic.<\/p>\n\n\n\n<p>(Shortform note: The model of Earth\u2019s interior as four uniform concentric layers is arguably obsolete. As scientists have gathered more and more seismograph data over the years and used increasingly sophisticated computer models to piece it together, <a href=\"https:\/\/www.sciencedaily.com\/releases\/2008\/05\/080501154212.htm\" target=\"_blank\" rel=\"noreferrer noopener\">they\u2019re developing a more detailed\u2014and more complex\u2014picture of the Earth\u2019s interior<\/a>. They\u2019ve found thin <a href=\"https:\/\/www.sciencedaily.com\/releases\/2005\/04\/050414110928.htm\" target=\"_blank\" rel=\"noreferrer noopener\">layers between some of the traditional layers<\/a> and <a href=\"https:\/\/www.sciencedaily.com\/releases\/2008\/03\/080310131507.htm\" target=\"_blank\" rel=\"noreferrer noopener\">an \u201cinner inner\u201d core inside the inner core<\/a>. They\u2019ve also found large lobes of dense material at the base of the mantle on opposite sides of the Earth. They\u2019ve even <a href=\"https:\/\/www.sciencedaily.com\/releases\/2018\/07\/180716114538.htm\" target=\"_blank\" rel=\"noreferrer noopener\">mapped out inverted mountain ranges on the bottom of the continental crust that appear to be made partially of solid diamond<\/a>.)<\/p>\n","protected":false},"excerpt":{"rendered":"<p>How much do we know about the interior parts of Earth? What are the current theories? Contrary to what you&#8217;ll see in sci-fi movies, nobody&#8217;s been to the center of the Earth. We can dig only so deep. So, scientists have to resort to some indirect ways of determining what&#8217;s far below the Earth&#8217;s surface. Continue reading to learn what scientists believe and why.<\/p>\n","protected":false},"author":9,"featured_media":90935,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_jetpack_memberships_contains_paid_content":false,"footnotes":""},"categories":[160],"tags":[886],"class_list":["post-90933","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-science","tag-a-short-history-of-nearly-everything","","tg-column-two"],"yoast_head":"<!-- This site is optimized with the Yoast SEO Premium plugin v24.3 (Yoast SEO v24.3) - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>The Interior Parts of Earth: What&#039;s Down Below the Surface? - Shortform Books<\/title>\n<meta name=\"description\" content=\"We know relatively little about the interior parts of Earth because we can\u2019t directly observe them. 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