{"id":5337,"date":"2015-01-27T15:24:40","date_gmt":"2015-01-27T15:24:40","guid":{"rendered":"https:\/\/www.open.ac.uk\/blogs\/per\/?p=5337"},"modified":"2015-05-06T13:09:38","modified_gmt":"2015-05-06T13:09:38","slug":"mercury-new-views-on-the-suns-most-innermost-planet","status":"publish","type":"post","link":"https:\/\/www.open.ac.uk\/blogs\/per\/?p=5337","title":{"rendered":"Mercury: new views on the Sun&#8217;s most innermost planet"},"content":{"rendered":"<div id=\"attachment_5339\" style=\"width: 310px\" class=\"wp-caption alignright\"><a href=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/SUPI-CEPSAR-2014_11.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-5339\" src=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/SUPI-CEPSAR-2014_11-300x200.jpg\" alt=\"Prof. David Rothery, The Open Univeristy, delivering his lecture\" width=\"300\" height=\"200\" class=\"size-medium wp-image-5339\" srcset=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/SUPI-CEPSAR-2014_11-300x200.jpg 300w, https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/SUPI-CEPSAR-2014_11-150x100.jpg 150w, https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/SUPI-CEPSAR-2014_11-1024x682.jpg 1024w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-5339\" class=\"wp-caption-text\">Prof. David Rothery, The Open University, delivering his lecture. Photo: Kate Bradshaw<\/p><\/div>\n<p>I\u2019m a geologist who now works mostly on other worlds, and the one that is keeping me busiest at present is Mercury. This is the closest planet to the Sun, which means that is always much closer to Earth than Jupiter ever gets. <\/p>\n<p>However, it is harder to study because the Sun\u2019s glare makes it difficult to observe with telescopes, and the Sun\u2019s gravity poses an enormous challenge if you want to get a spacecraft into orbit about Mercury. <\/p>\n<p>NASA achieved this with its <a href=\"http:\/\/messenger.jhuapl.edu\/\" title=\"MESSENGER\">MESSENGER<\/a> orbiter (2011-2015), and I\u2019m on the science team for the European Space Agency\u2019s <a href=\"http:\/\/www.cosmos.esa.int\/web\/bepicolombo\" title=\"BepiColombo\">BepiColombo<\/a> orbiter 2024-2025, due for launch in later 2016.<\/p>\n<p><strong>2015 Science Matters Lecture<\/strong><br \/>\nI recently introduced school students, teachers and members of the public from Milton Keynes to my research at the 2015 Science Matters lectures. <\/p>\n<p>You can watch a recording of my talk below.<\/p>\n<p><iframe loading=\"lazy\" src=\"http:\/\/player.open.ac.uk\/embed\/c3bdf54896\" height=\"270\" width=\"480\" frameborder=\"0\" allowfullscreen ><\/iframe> <\/p>\n<p><!--more--><\/p>\n<p><strong>What do we know about the planet Mercury?<\/strong><br \/>\nThere are many reasons why Mercury is turning out to be special. For one thing, its closeness to the Sun means that it experiences similar conditions to those affecting the most easily detected planets of other stars, known as <a href=\"https:\/\/www.open.ac.uk\/blogs\/per\/?p=1800\" title=\"exoplanets\">exoplanets<\/a>. <\/p>\n<div id=\"attachment_5368\" style=\"width: 600px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/rocky-planets.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-5368\" src=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/rocky-planets-1024x363.jpg\" alt=\"The rocky (terrestrial) planets plus the Moon, all to scale. From left to right: Mercury, Venus, Earth, Moon, Mars.\" width=\"590\" height=\"195\" class=\"size-large wp-image-5368\" \/><\/a><p id=\"caption-attachment-5368\" class=\"wp-caption-text\">The rocky (terrestrial) planets plus the Moon, all to scale. From left to right: Mercury, Venus, Earth, Moon, Mars.<\/p><\/div>\n<p>Mercury is the only rocky planet other than the Earth to generate its own magnetic field, so there must be a liquid, molten, zone in its iron-rich core. <\/p>\n<div id=\"attachment_5372\" style=\"width: 310px\" class=\"wp-caption alignright\"><a href=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/core.png\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-5372\" src=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/core-300x292.png\" alt=\"Mercury\u2019s probable internal structure (Rothery, 2015)\" width=\"300\" height=\"292\" class=\"size-medium wp-image-5372\" srcset=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/core-300x292.png 300w, https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/core-150x146.png 150w, https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/core.png 757w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-5372\" class=\"wp-caption-text\">Mercury\u2019s probable internal structure (Rothery, 2015)<\/p><\/div>\n<p>Mercury is a dense planet, so its core must make up a much greater proportion of the planet\u2019s volume than in the case of the Earth.<\/p>\n<p>In fact, the rocky mantle and crust surrounding Mercury\u2019s core is probably not much more than 400 km thick. The rocky surface appears to have been formed by a succession of giant volcanic lava flows, most of which happened billions of years ago so that there has been plenty of time for vast numbers of impact craters to form as a result of bombardment by asteroids and comets.<\/p>\n<p>The comparatively small amount of rock surrounding the core compared to the other rocky planets suggests that Mercury had a violent birth, in which most of its original rock was stripped away \u2013 perhaps as the result of an enormous collision with another planet. <\/p>\n<div id=\"attachment_5389\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/Mercury.png\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-5389\" src=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/Mercury-1024x673.png\" alt=\"1700 km wide view from MESSENGER, including the edge of Mercury\u2019s northern volcanic plains (NASA\/JHUAPL\/CIW)\" width=\"640\" height=\"420\" class=\"size-large wp-image-5389\" srcset=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/Mercury-1024x673.png 1024w, https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/Mercury-150x98.png 150w, https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/Mercury-300x197.png 300w, https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/Mercury.png 1275w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><\/a><p id=\"caption-attachment-5389\" class=\"wp-caption-text\">1700 km wide view from MESSENGER, including the edge of Mercury\u2019s northern volcanic plains (NASA\/JHUAPL\/CIW)<\/p><\/div>\n<p><strong>The significance of NASA&#8217;s MESSENGER orbiter<\/strong><br \/>\nThis idea has been severely challenged by MESSENGER data, which show that Mercury is rich in volatile elements of the kind that would have been most easily lost during hot, violent events. For example:<\/p>\n<ul>\n<li>wherever MESSENGER looked, the surface has 2-5% sulfur;<\/li>\n<li>the ratio of potassium to thorium is high;\n<\/li>\n<li>there are places where patches on the surface seem to have been vaporized;\n<\/li>\n<li>and the globe is peppered with volcanic vents where explosive eruptions have happened, driven by violent expansion of gas bubbles in the magma. <\/li>\n<\/ul>\n<p><strong>What don&#8217;t we (yet) know about the planet Mercury?<\/strong><br \/>\nOne of the joys of conducting research is finding out new things. For example:<\/p>\n<ul>\n<li>we don\u2019t know what has been removed from the vaporized patches of surface;\n<\/li>\n<li>we don\u2019t know what the gases were that drove the explosive eruptions;\n<\/li>\n<li>and we don\u2019t know whether the sulfur occurs as elemental sulfur or in compounds such as magnesium or calcium sulfide.<\/li>\n<\/ul>\n<p>We also don\u2019t know when the most recent volcanic explosions occurred, but work by <a href=\"http:\/\/www.open.ac.uk\/people\/rt4949\" title=\"Rebecca Thomas\">Rebecca Thomas<\/a>, one of my students, suggests that activity continued into the past <a href=\"http:\/\/www.astrobio.net\/news-exclusive\/violent-eruptions-mercurys-past-hold-clues-formation\/\" title=\"billion years\">billion years<\/a>.<\/p>\n<div id=\"attachment_5391\" style=\"width: 570px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/Mercury_blue.png\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-5391\" src=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/Mercury_blue.png\" alt=\"910 km MESSENGER view of Mercury. The large yellow spot at top right is a deposit from an explosive volcanic eruption from the deeply-shadowed vent at its centre. The smaller yellow spot in below the middle of the frame is a similar deposit, from a vent too small to make out. (NASA\/JHUAPL\/CIW)\" width=\"580\" height=\"464\" class=\"size-full wp-image-5391\" srcset=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/Mercury_blue-150x120.png 150w, https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/Mercury_blue-300x241.png 300w\" sizes=\"auto, (max-width: 580px) 100vw, 580px\" \/><\/a><p id=\"caption-attachment-5391\" class=\"wp-caption-text\">910 km MESSENGER view of Mercury. The large yellow spot at top right is a deposit from an explosive volcanic eruption from the deeply-shadowed vent at its centre. The smaller yellow spot in below the middle of the frame is a similar deposit, from a vent too small to make out. (NASA\/JHUAPL\/CIW)<\/p><\/div>\n<p><strong>Locating Mercury in the night sky<\/strong><br \/>\nMercury is hard to see for yourself. You&#8217;ll have a chance to see the planet in late April-early May 2015, when Mercury will be slightly higher on the evening sky after sunset. See <a href=\"http:\/\/earthsky.org\/space\/animation-shows-venus-in-evening-sky-late-2014-and-2015\" title=\"here\">here<\/a> for an animation of Mercury and other planets in the evening sky of early 2015. <\/p>\n<p>An even better chance, of a different kind, will be 12:12-19:42 BST on Monday 9 May 2016 when Mercury will cross the face of the Sun. <a href=\"http:\/\/www.astromediashop.co.uk\/Astronomy_files\/The Solar Projector.pdf\" title=\"Simple equipment\">Simple equipment<\/a> will enable to see it then in silhouette. I hope also to be able to stream live images on the internet from at least one ESA satellite, and to make the day a <a href=\"http:\/\/www.cosmos.esa.int\/web\/bepicolombo\/mercury-transit\" title=\"Europe-wide Mercury party\">Europe-wide Mercury party<\/a> as part of the build up towards the launch of BepiColombo.<\/p>\n<hr\/>\n<div id=\"attachment_5361\" style=\"width: 122px\" class=\"wp-caption alignright\"><a href=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/Dave.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-5361\" src=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/Dave-112x150.jpg\" alt=\"Prof. David Rothery, The Open University\" width=\"112\" height=\"150\" class=\"size-thumbnail wp-image-5361\" srcset=\"https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/Dave-112x150.jpg 112w, https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/Dave-225x300.jpg 225w, https:\/\/www.open.ac.uk\/blogs\/per\/wp-content\/uploads\/2015\/01\/Dave.jpg 720w\" sizes=\"auto, (max-width: 112px) 100vw, 112px\" \/><\/a><p id=\"caption-attachment-5361\" class=\"wp-caption-text\">Prof. David Rothery, The Open University<\/p><\/div>\n<p>If you share my passion for planets, you might be interested in my nice and cheap <a href=\"http:\/\/ukcatalogue.oup.com\/product\/9780199573509.do\" title=\"Very Short Introduction to Planets\">Very Short Introduction to Planets<\/a>.<\/p>\n<p>Alternatively, if you want to read about Mercury in greater depth then seek out <a href=\"http:\/\/www.springer.com\/astronomy\/astronomy%2C+observations+and+techniques\/book\/978-3-319-12116-1\" title=\"Planet Mercury: from Pale Pink Dot to Dynamic World\">Planet Mercury: from Pale Pink Dot to Dynamic World<\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>I\u2019m a geologist who now works mostly on other worlds, and the one that is keeping me busiest at present is Mercury. This is the closest planet to the Sun, which means that is always much closer to Earth than &hellip; <a href=\"https:\/\/www.open.ac.uk\/blogs\/per\/?p=5337\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":54,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[16,48],"tags":[56,39,24,41,103,126,55,127,22,49,23],"class_list":["post-5337","post","type-post","status-publish","format-standard","hentry","category-events","category-school-university-engagement","tag-cepsar","tag-denbigh-school","tag-engaging-opportunities","tag-engaging-with-school-students","tag-esa","tag-geology","tag-lecture","tag-nasa","tag-nccpe","tag-rcuk","tag-supi"],"_links":{"self":[{"href":"https:\/\/www.open.ac.uk\/blogs\/per\/index.php?rest_route=\/wp\/v2\/posts\/5337","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.open.ac.uk\/blogs\/per\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.open.ac.uk\/blogs\/per\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.open.ac.uk\/blogs\/per\/index.php?rest_route=\/wp\/v2\/users\/54"}],"replies":[{"embeddable":true,"href":"https:\/\/www.open.ac.uk\/blogs\/per\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=5337"}],"version-history":[{"count":70,"href":"https:\/\/www.open.ac.uk\/blogs\/per\/index.php?rest_route=\/wp\/v2\/posts\/5337\/revisions"}],"predecessor-version":[{"id":5715,"href":"https:\/\/www.open.ac.uk\/blogs\/per\/index.php?rest_route=\/wp\/v2\/posts\/5337\/revisions\/5715"}],"wp:attachment":[{"href":"https:\/\/www.open.ac.uk\/blogs\/per\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=5337"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.open.ac.uk\/blogs\/per\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=5337"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.open.ac.uk\/blogs\/per\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=5337"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}