{"id":5129,"date":"2015-06-29T04:00:43","date_gmt":"2015-06-29T09:00:43","guid":{"rendered":"http:\/\/gisgeography.com\/?p=5129"},"modified":"2025-04-17T05:37:53","modified_gmt":"2025-04-17T10:37:53","slug":"magnetic-north-vs-geographic-true-pole","status":"publish","type":"post","link":"https:\/\/gisgeography.com\/magnetic-north-vs-geographic-true-pole\/","title":{"rendered":"Magnetic North vs Geographic (True) North Pole"},"content":{"rendered":"\n<figure class=\"wp-block-image\"><img loading=\"lazy\" decoding=\"async\" width=\"1265\" height=\"843\" src=\"https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/compass-653307_1280-1265x843.jpg\" alt=\"Compass Direction\" class=\"wp-image-5002\" srcset=\"https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/compass-653307_1280-1265x843.jpg 1265w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/compass-653307_1280-300x200.jpg 300w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/compass-653307_1280-678x452.jpg 678w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/compass-653307_1280-768x512.jpg 768w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/compass-653307_1280-50x33.jpg 50w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/compass-653307_1280-150x100.jpg 150w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/compass-653307_1280-200x133.jpg 200w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/compass-653307_1280-425x283.jpg 425w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/compass-653307_1280-550x367.jpg 550w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/compass-653307_1280-115x77.jpg 115w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/compass-653307_1280-850x566.jpg 850w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/compass-653307_1280-233x155.jpg 233w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/compass-653307_1280.jpg 1280w\" sizes=\"auto, (max-width: 1265px) 100vw, 1265px\" \/><\/figure>\n\n\n\n<div class=\"wp-block-group\" style=\"padding-top:var(--wp--preset--spacing--40);padding-bottom:var(--wp--preset--spacing--40)\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<hr class=\"wp-block-separator has-css-opacity is-style-default\"\/>\n\n\n\n<blockquote class=\"wp-block-quote has-text-align-center is-style-large is-layout-flow wp-block-quote-is-layout-flow\">\n<p>&#8220;Standing exactly on the North Pole, which direction would the compass point?&#8221;<\/p>\n<\/blockquote>\n\n\n\n<hr class=\"wp-block-separator has-css-opacity is-style-default\"\/>\n\n\n\n<h3 class=\"wp-block-heading\">The Story of the Explorer&#8217;s Compass<\/h3>\n\n\n\n<p>Imagine. You are an explorer standing <strong>exactly on the North Pole<\/strong>.<\/p>\n\n\n\n<p>It&#8217;s been a long journey and it&#8217;s freezing cold.<\/p>\n\n\n\n<p>You pull out your compass.<\/p>\n\n\n\n<p>What <strong>direction<\/strong> would the needle on the compass point?<\/p>\n\n\n\n<p>The answer may not be what you think.<\/p>\n\n\n\n<p>In order to answer this question, you will have to understand the difference between the <strong>true geographic north<\/strong> and <strong>magnetic north<\/strong>.<\/p>\n\n\n\n<p>Because these two north locations are completely different.<\/p>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-group\" style=\"padding-top:var(--wp--preset--spacing--40);padding-bottom:var(--wp--preset--spacing--40)\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<h3 class=\"wp-block-heading\">What is the Geographic (True) North Pole?<\/h3>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"alignright\"><img loading=\"lazy\" decoding=\"async\" width=\"298\" height=\"300\" src=\"https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Longitude-298x300.png\" alt=\"Longitude\" class=\"wp-image-22455\" srcset=\"https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Longitude-298x300.png 298w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Longitude-150x150.png 150w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Longitude-50x50.png 50w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Longitude-200x200.png 200w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Longitude-422x425.png 422w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Longitude-115x116.png 115w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Longitude.png 446w\" sizes=\"auto, (max-width: 298px) 100vw, 298px\" \/><\/figure>\n<\/div>\n\n\n<p>The Earth rotates on the geographic north and south poles. The geographic north and south poles are where <a href=\"http:\/\/gisgeography.com\/latitude-longitude-coordinates\/\" target=\"_blank\" rel=\"noopener noreferrer\">lines of longitude<\/a> (meridians) <strong>converge in the north<\/strong>. The south and north poles are directly opposite to one another.<\/p>\n\n\n\n<p>The North Pole is located in the middle of the <a href=\"https:\/\/gisgeography.com\/arctic-maps-help-explain\/\">Arctic Ocean<\/a>. Scientists have tried marking the North Pole. Because the water here is permanently covered with <strong>moving sea ice<\/strong>, it&#8217;s practically impossible to construct any type of permanent station at the true North Pole.<\/p>\n\n\n\n<p>On the other side of the Earth, the South Pole lies on a <strong>continental land mass<\/strong> known as Antarctica. Because the ice on top of <a href=\"https:\/\/gisgeography.com\/antarctica-map-satellite-image\/\">Antarctica<\/a> moves only a few meters a year, the United States Antarctica program has installed a marker here to delineate the true South Pole.<\/p>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-group\" style=\"padding-top:var(--wp--preset--spacing--40);padding-bottom:var(--wp--preset--spacing--40)\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<h3 class=\"wp-block-heading\">What is the Magnetic North Pole?<\/h3>\n\n\n\n<p>The Earth is one <strong>big magnet<\/strong>. The Magnetic North Pole (also known as the <em>North Dip Pole<\/em>) is a point on <strong>Ellesmere Island in Northern Canada<\/strong> where the northern lines of attraction enter the Earth.<\/p>\n\n\n\n<p>A compass needle rests freely in its casing so it can maneuver itself. When you pull out a compass, it <strong>aligns itself with the Earth&#8217;s magnetic field<\/strong>. The small magnetic pin is how a compass responds to Earth&#8217;s magnetism.<\/p>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter\"><img loading=\"lazy\" decoding=\"async\" width=\"425\" height=\"299\" src=\"https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Earth-Magnetic-Field-425x299.png\" alt=\"Earth Magnetic Field\" class=\"wp-image-5936\" srcset=\"https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Earth-Magnetic-Field-425x299.png 425w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Earth-Magnetic-Field-300x211.png 300w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Earth-Magnetic-Field-678x477.png 678w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Earth-Magnetic-Field-768x541.png 768w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Earth-Magnetic-Field-50x35.png 50w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Earth-Magnetic-Field-200x141.png 200w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Earth-Magnetic-Field-550x387.png 550w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Earth-Magnetic-Field-115x81.png 115w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Earth-Magnetic-Field-220x155.png 220w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Earth-Magnetic-Field.png 797w\" sizes=\"auto, (max-width: 425px) 100vw, 425px\" \/><\/figure>\n<\/div>\n\n\n<p>This means that a compass needle will point to the Magnetic North Pole &#8211; which is different from the geographic north.<\/p>\n\n\n\n<p>But how much of a difference is the magnetic north vs. geographic north?<\/p>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-group\" style=\"padding-top:var(--wp--preset--spacing--40);padding-bottom:var(--wp--preset--spacing--40)\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<h3 class=\"wp-block-heading\">Where are the Magnetic North Pole and Geographic North Pole?<\/h3>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"alignright\"><img loading=\"lazy\" decoding=\"async\" width=\"300\" height=\"297\" src=\"https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Magnetic-North-300x297.png\" alt=\"Magnetic North\" class=\"wp-image-22447\" srcset=\"https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Magnetic-North-300x297.png 300w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Magnetic-North-150x150.png 150w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Magnetic-North-50x50.png 50w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Magnetic-North-200x198.png 200w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Magnetic-North-115x114.png 115w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Magnetic-North.png 350w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/figure>\n<\/div>\n\n\n<p>The question is:<\/p>\n\n\n\n<p>Where would a compass needle point if you were standing on the true North Pole?<\/p>\n\n\n\n<p>If you were standing on the geographic north pole holding your compass, it would point towards northern Canada at Ellesmere Island. This is a difference of about 500 kilometers between the Geographic North and Magnetic North poles!<\/p>\n\n\n\n<p>This difference is called the <strong>magnetic inclination<\/strong>. <em>Magnetic deviation<\/em> is the error of a compass needle including nearby metallic objects.<\/p>\n\n\n\n<p>Magnetic inclination varies according to where you are located on the globe. In order to point you in the right direction, users can compensate for magnetic inclination by using charts of declination or local calibration.<\/p>\n\n\n<style>.kb-row-layout-wrap.wp-block-kadence-rowlayout.kb-row-layout-id5129_5c1eb4-f814{margin-top:var(--global-kb-spacing-md, 2rem);margin-bottom:var(--global-kb-spacing-md, 2rem);}.kb-row-layout-id5129_5c1eb4-f814 > .kt-row-column-wrap{align-content:start;}:where(.kb-row-layout-id5129_5c1eb4-f814 > .kt-row-column-wrap) > .wp-block-kadence-column{justify-content:start;}.kb-row-layout-id5129_5c1eb4-f814 > .kt-row-column-wrap{column-gap:var(--global-kb-gap-md, 2rem);row-gap:var(--global-kb-gap-md, 2rem);max-width:1000px;margin-left:auto;margin-right:auto;padding-top:var(--global-kb-spacing-xl, 4rem);padding-right:var(--global-kb-spacing-md, 2rem);padding-bottom:var(--global-kb-spacing-xl, 4rem);padding-left:var(--global-kb-spacing-md, 2rem);grid-template-columns:minmax(0, 1fr);}.kb-row-layout-id5129_5c1eb4-f814 > .kt-row-layout-overlay{opacity:0.30;}@media all and (max-width: 1024px){.kb-row-layout-id5129_5c1eb4-f814 > .kt-row-column-wrap{grid-template-columns:minmax(0, 1fr);}}@media all and (max-width: 767px){.kb-row-layout-id5129_5c1eb4-f814 > .kt-row-column-wrap{grid-template-columns:minmax(0, 1fr);}}<\/style><div class=\"kb-row-layout-wrap kb-row-layout-id5129_5c1eb4-f814 alignnone has-theme-palette8-background-color kt-row-has-bg wp-block-kadence-rowlayout\"><div class=\"kt-row-column-wrap kt-has-1-columns kt-row-layout-equal kt-tab-layout-inherit kt-mobile-layout-row kt-row-valign-top\">\n<style>.kadence-column5129_de61df-d213 > .kt-inside-inner-col,.kadence-column5129_de61df-d213 > .kt-inside-inner-col:before{border-top-left-radius:0px;border-top-right-radius:0px;border-bottom-right-radius:0px;border-bottom-left-radius:0px;}.kadence-column5129_de61df-d213 > .kt-inside-inner-col{column-gap:var(--global-kb-gap-sm, 1rem);}.kadence-column5129_de61df-d213 > .kt-inside-inner-col{flex-direction:column;}.kadence-column5129_de61df-d213 > .kt-inside-inner-col > .aligncenter{width:100%;}.kadence-column5129_de61df-d213 > .kt-inside-inner-col:before{opacity:0.3;}.kadence-column5129_de61df-d213{text-align:center;}.kadence-column5129_de61df-d213{position:relative;}@media all and (max-width: 1024px){.kadence-column5129_de61df-d213 > .kt-inside-inner-col{flex-direction:column;justify-content:center;}}@media all and (max-width: 767px){.kadence-column5129_de61df-d213 > .kt-inside-inner-col{flex-direction:column;justify-content:center;}}.kadence-column5129_de61df-d213 {}<\/style>\n<div class=\"wp-block-kadence-column kadence-column5129_de61df-d213 inner-column-1\"><div class=\"kt-inside-inner-col\"><style>.wp-block-kadence-advancedheading.kt-adv-heading5129_f396d8-5311, .wp-block-kadence-advancedheading.kt-adv-heading5129_f396d8-5311[data-kb-block=\"kb-adv-heading5129_f396d8-5311\"]{text-align:center;font-size:var(--global-kb-font-size-sm, 0.9rem);font-style:normal;text-transform:uppercase;}.wp-block-kadence-advancedheading.kt-adv-heading5129_f396d8-5311 mark.kt-highlight, .wp-block-kadence-advancedheading.kt-adv-heading5129_f396d8-5311[data-kb-block=\"kb-adv-heading5129_f396d8-5311\"] mark.kt-highlight{font-style:normal;color:#f76a0c;-webkit-box-decoration-break:clone;box-decoration-break:clone;padding-top:0px;padding-right:0px;padding-bottom:0px;padding-left:0px;}.wp-block-kadence-advancedheading.kt-adv-heading5129_f396d8-5311 img.kb-inline-image, .wp-block-kadence-advancedheading.kt-adv-heading5129_f396d8-5311[data-kb-block=\"kb-adv-heading5129_f396d8-5311\"] img.kb-inline-image{width:150px;vertical-align:baseline;}<\/style>\n<h6 class=\"kt-adv-heading5129_f396d8-5311 wp-block-kadence-advancedheading\" data-kb-block=\"kb-adv-heading5129_f396d8-5311\">NOTE<\/h6>\n\n\n<style>.wp-block-kadence-advancedheading.kt-adv-heading5129_606484-6112, .wp-block-kadence-advancedheading.kt-adv-heading5129_606484-6112[data-kb-block=\"kb-adv-heading5129_606484-6112\"]{text-align:center;font-size:26px;line-height:1.2;font-style:normal;}.wp-block-kadence-advancedheading.kt-adv-heading5129_606484-6112 mark.kt-highlight, .wp-block-kadence-advancedheading.kt-adv-heading5129_606484-6112[data-kb-block=\"kb-adv-heading5129_606484-6112\"] mark.kt-highlight{font-style:normal;color:#f76a0c;-webkit-box-decoration-break:clone;box-decoration-break:clone;padding-top:0px;padding-right:0px;padding-bottom:0px;padding-left:0px;}.wp-block-kadence-advancedheading.kt-adv-heading5129_606484-6112 img.kb-inline-image, .wp-block-kadence-advancedheading.kt-adv-heading5129_606484-6112[data-kb-block=\"kb-adv-heading5129_606484-6112\"] img.kb-inline-image{width:150px;vertical-align:baseline;}@media all and (max-width: 1024px){.wp-block-kadence-advancedheading.kt-adv-heading5129_606484-6112, .wp-block-kadence-advancedheading.kt-adv-heading5129_606484-6112[data-kb-block=\"kb-adv-heading5129_606484-6112\"]{font-size:36px;}}@media all and (max-width: 767px){.wp-block-kadence-advancedheading.kt-adv-heading5129_606484-6112, .wp-block-kadence-advancedheading.kt-adv-heading5129_606484-6112[data-kb-block=\"kb-adv-heading5129_606484-6112\"]{font-size:26px;line-height:1.2;}}<\/style>\n<h3 class=\"kt-adv-heading5129_606484-6112 wp-block-kadence-advancedheading\" data-kb-block=\"kb-adv-heading5129_606484-6112\">The difference today is about 500 kilometers. But the Magnetic North Pole is actually moving kilometers every year. This phenomenon is known as the Polar Shift Theory.<\/h3>\n<\/div><\/div>\n\n<\/div><\/div><\/div><\/div>\n\n\n\n<div class=\"wp-block-group\" style=\"padding-top:var(--wp--preset--spacing--40);padding-bottom:var(--wp--preset--spacing--40)\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<h3 class=\"wp-block-heading\">Polar Shift Theory: Earth&#8217;s Ever-Changing Magnetic North Pole<\/h3>\n\n\n\n<figure class=\"wp-block-image\"><img loading=\"lazy\" decoding=\"async\" width=\"425\" height=\"272\" src=\"https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/Magnetic-North-Shift-NOAA-425x272.png\" alt=\"Magnetic North Shift\" class=\"wp-image-5001\" srcset=\"https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/Magnetic-North-Shift-NOAA-425x272.png 425w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/Magnetic-North-Shift-NOAA-300x192.png 300w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/Magnetic-North-Shift-NOAA-50x32.png 50w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/Magnetic-North-Shift-NOAA-200x128.png 200w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/Magnetic-North-Shift-NOAA-115x74.png 115w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/Magnetic-North-Shift-NOAA.png 500w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/05\/Magnetic-North-Shift-NOAA-242x155.png 242w\" sizes=\"auto, (max-width: 425px) 100vw, 425px\" \/><\/figure>\n\n\n\n<p>The world we live in is dynamic. Earth is changing every day.<\/p>\n\n\n\n<p>Plate tectonics push continents apart, sea levels fluctuate up and down, and volcanoes erupt discharging ash and smoke&#8230;<\/p>\n\n\n\n<p>These are examples of natural phenomena that occur in cycles and are dynamic on our planet. The location of our <strong>magnetic north<\/strong> is really no different.<\/p>\n\n\n\n<p>Over the last 150 years, the magnetic pole has crept north over 1000 kilometers. Scientists suggest it migrates about 10 kilometers yearly and can even flip from pole to pole. Several years ago, the speed had <a href=\"http:\/\/science.nasa.gov\/science-news\/science-at-nasa\/2003\/29dec_magneticfield\/\" target=\"_blank\" rel=\"noopener noreferrer\">accelerated to about 40 kilometers<\/a> per year and could reach Siberia in a few decades.<\/p>\n\n\n\n<p><a href=\"http:\/\/maps.ngdc.noaa.gov\/viewers\/historical_declination\/\" target=\"_blank\" rel=\"noopener noreferrer\">NOAA&#8217;s historical declination map<\/a> shows lines of constant magnetic declination (isogonic lines). Isogonic lines indicate what direction compass needles will point &#8211; along the lines of magnetic force.<\/p>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-group\" style=\"padding-top:var(--wp--preset--spacing--40);padding-bottom:var(--wp--preset--spacing--40)\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<h3 class=\"wp-block-heading\">Polar Reversals: South-Pole Pointing Compass<\/h3>\n\n\n\n<p>Imagine your compass pointing south instead of north. If you were alive to see it 800,000 years ago, it would have been the <strong>Magnetic South Pole<\/strong>.<\/p>\n\n\n\n<p>It takes <a href=\"https:\/\/climate.nasa.gov\/explore\/ask-nasa-climate\/3104\/flip-flop-why-variations-in-earths-magnetic-field-arent-causing-todays-climate-change\/\" target=\"_blank\" rel=\"noreferrer noopener\">200,000 to 300,000 years for Earth&#8217;s magnetic field to flip polarity<\/a>. Flipping polarity means the lines of attraction that enter the Earth would flip north to the south pole, or vice versa.<\/p>\n\n\n\n<p>This means that it has been twice that long since the last reversal. Some believe we are long overdue for a pole reversal.<\/p>\n\n\n\n<p>But there&#8217;s really no need to panic:<\/p>\n\n\n\n<p>NASA scientists say a reversal happens over hundreds or thousands of years. It&#8217;s <strong>not exactly a clean backflip<\/strong> that happens like a flick of a switch.<\/p>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-group\" style=\"padding-top:var(--wp--preset--spacing--40);padding-bottom:var(--wp--preset--spacing--40)\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<h3 class=\"wp-block-heading\">Why Does the Earth Have a Magnetic Field in the First Place?<\/h3>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"alignright\"><img loading=\"lazy\" decoding=\"async\" width=\"290\" height=\"300\" src=\"https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Inner-Earth-290x300.png\" alt=\"Inner Earth\" class=\"wp-image-22458\" srcset=\"https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Inner-Earth-290x300.png 290w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Inner-Earth-48x50.png 48w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Inner-Earth-193x200.png 193w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Inner-Earth-115x119.png 115w, https:\/\/gisgeography.com\/wp-content\/uploads\/2015\/06\/Inner-Earth.png 407w\" sizes=\"auto, (max-width: 290px) 100vw, 290px\" \/><\/figure>\n<\/div>\n\n\n<p>Geophysicists believe Earth&#8217;s magnetic field presence is because of what&#8217;s inside Earth.<\/p>\n\n\n\n<p>The Earth consists of a <strong>solid iron core<\/strong>. Surrounding the iron core is an ocean of <strong>hot, liquid metal<\/strong>. The liquid metal that flows in Earth&#8217;s core creates electrical currents, which in turn create our magnetic field.<\/p>\n\n\n\n<p>Unlike a solid fridge magnet, the liquid metal surrounding the inner core moves freely. This explains why the magnetic pole can migrate.<\/p>\n\n\n\n<p>Although geophysicists cannot measure the inner core directly, this is why there is a strong belief that the matter governing Earth&#8217;s magnetic field moves around.<\/p>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-group\" style=\"padding-top:var(--wp--preset--spacing--40);padding-bottom:var(--wp--preset--spacing--40)\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<h3 class=\"wp-block-heading\">Magnets, Compasses, and North Bearings<\/h3>\n\n\n\n<p>Today, the Geographic North Pole differs from the Magnetic North Pole by about 500 kilometers. But it&#8217;s changing every day.<\/p>\n\n\n\n<p>The Geographic North Pole is where lines of longitudes converge into what we call the North Pole. The Magnetic Pole is a point in Northern Canada where the northern lines of attraction enter the Earth.<\/p>\n\n\n\n<p>A compass needle will point to the direction of the Magnetic North Pole. But this doesn&#8217;t mean that a compass always points to the Geographic North Pole. This difference is magnetic inclination.<\/p>\n\n\n\n<p>The Earth&#8217;s magnetic north is changing every day because of the hot, liquid metal that surrounds the inner core. It can change so much that the Earth&#8217;s magnetic field can flip polarity. This is called the <em>Polar Reversal Theory<\/em>.<\/p>\n\n\n\n<p>Next time you&#8217;re out in the woods with your compass, don&#8217;t forget about the small magnetic pin that moves freely in the direction of the <strong>Magnetic North Pole<\/strong>.<\/p>\n<\/div><\/div>\n","protected":false},"excerpt":{"rendered":"<p>The Magnetic North Pole is a point in Northern Canada where the northern lines of attraction enter the Earth.  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