{"id":792271,"date":"2024-12-26T06:56:03","date_gmt":"2024-12-26T11:56:03","guid":{"rendered":"http:\/\/spaceweekly.com\/?p=792271"},"modified":"2024-12-26T06:56:03","modified_gmt":"2024-12-26T11:56:03","slug":"ios-raging-volcanoes-are-self-powered","status":"publish","type":"post","link":"https:\/\/spaceweekly.com\/?p=792271","title":{"rendered":"Io\u2019s raging volcanoes are self-powered"},"content":{"rendered":"<p> <br \/>\n<\/p>\n<div>\n<figure id=\"attachment_496747\" aria-describedby=\"caption-attachment-496747\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><figcaption id=\"caption-attachment-496747\" class=\"wp-caption-text\">View larger. | NASA\u2019s Juno spacecraft captured this view of Io on December 30, 2023. A new NASA study suggested Io doesn\u2019t have a global subsurface ocean of magma. Rather, each of Io\u2019s raging volcanoes is self-powered with its own magma pool. Image via NASA\/ JPL-Caltech\/ SwRI\/ MSSS\/ Gerald Eichst\u00e4dt.<\/figcaption><\/figure>\n<ul>\n<li><strong>Jupiter\u2019s moon Io is the most volcanically active world<\/strong> in the entire solar system. It has at least 400 known active volcanoes. So, where does its magma come from?<\/li>\n<li><strong>There might be a subsurface global ocean of magma,<\/strong> scientists have theorized. Or is the magma in smaller pockets?<\/li>\n<li><strong>There is no global magma ocean<\/strong>, said a new study of data from NASA\u2019s Juno spacecraft. Instead, each volcano has its own localized pool of magma.<\/li>\n<\/ul>\n<p>The 2025 EarthSky lunar calendar makes a great gift. Get yours today!<\/p>\n<h3>Io\u2019s raging volcanoes have their own magma power sources<\/h3>\n<p>Jupiter\u2019s moon Io is a world of volcanoes. In fact, it is the most volcanic body in the entire solar system. But how did it become that way? We know Jupiter\u2019s powerful gravitational pull heats Io\u2019s interior, melting rock and feeding the 400 known volcanoes. But is there a global ocean of magma beneath the surface? Or does each volcano have its own lava pool? Scientists with NASA\u2019s Juno mission said on December 12, 2024, that it\u2019s likely the latter. Io\u2019s raging volcanoes are self-powered.<\/p>\n<p>The researchers published their peer-reviewed paper in <em>Nature<\/em> on December 12, 2024. While peer-reviewed and accepted for publication, the paper is a preview version and still undergoing editing.<\/p>\n<p>The results were also discussed at the American Geophysical Union\u2019s annual meeting this month in Washington, D.C.<\/p>\n<h3>Does Io have a magma ocean?<\/h3>\n<p>With Io having so many volcanoes \u2013 at least 400 known \u2013 scientists theorized there might be a global ocean of magma beneath the surface. Many of the volcanoes are active at any given time, blasting lava and plumes into the extremely thin atmosphere. So there must be an on-going supply of magma below ground. Imaging scientist Linda Morabito at NASA\u2019s Jet Propulsion Laboratory (JPL) in California first saw signs of volcanic activity in Voyager 1 images in 1979.<\/p>\n<p>But is that magma global, or is it localized beneath each volcano?<\/p>\n<p>Scott Bolton is the principal investigator for the Juno mission. He said:<\/p>\n<blockquote>\n<p>Since Morabito\u2019s discovery, planetary scientists have wondered how the volcanoes were fed from the lava underneath the surface. Was there a shallow ocean of white-hot magma fueling the volcanoes, or was their source more localized? We knew data from Juno\u2019s two very close flybys could give us some insights on how this tortured moon actually worked.<\/p>\n<\/blockquote>\n<p>So, does Io have a magma ocean? The answer appears to be no.<\/p>\n<figure id=\"attachment_496897\" aria-describedby=\"caption-attachment-496897\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/earthsky.org\/upl\/2024\/12\/Io-volcanoes-infrared-Juno-July-5-2022.jpg\" alt=\"Red sphere, partly in shadow, on black background. There are many small, very bright spots on its surface.\" width=\"800\" height=\"801\" class=\"size-full wp-image-496897\" srcset=\"https:\/\/earthsky.org\/upl\/2024\/12\/Io-volcanoes-infrared-Juno-July-5-2022.jpg 800w, https:\/\/earthsky.org\/upl\/2024\/12\/Io-volcanoes-infrared-Juno-July-5-2022-300x300.jpg 300w, https:\/\/earthsky.org\/upl\/2024\/12\/Io-volcanoes-infrared-Juno-July-5-2022-150x150.jpg 150w, https:\/\/earthsky.org\/upl\/2024\/12\/Io-volcanoes-infrared-Juno-July-5-2022-768x769.jpg 768w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\"\/><figcaption id=\"caption-attachment-496897\" class=\"wp-caption-text\">View larger. | NASA\u2019s Juno spacecraft captured this stunning infrared view of Io and its many volcanoes on July 5, 2022. Image via NASA\/ JPL-Caltech\/ SwRI\/ ASI\/ INAF\/ JIRAM.<\/figcaption><\/figure>\n<h3>Io\u2019s raging volcanoes are self-powered<\/h3>\n<p>Juno, which orbits Jupiter, made extremely close flybys of Io in December 2023 and February 2024. It came within 930 miles (1,500 km) of the scorched and roiling surface. Juno measured Io\u2019s gravity by calculating how it affected the spacecraft\u2019s acceleration. This can provide clues about the moon\u2019s interior.<\/p>\n<p>Io experiences what scientists call tidal flexing, or tidal heating. That\u2019s due to Jupiter\u2019s gravity squeezing and pulling on Io\u2019s insides. This creates heat and melts subsurface rock, forming magma. The scientists wanted to know if that subsurface magma was global or just under each volcano. Bolton explained:<\/p>\n<blockquote>\n<p>This constant flexing creates immense energy, which literally melts portions of Io\u2019s interior. If Io has a global magma ocean, we knew the signature of its tidal deformation would be much larger than a more rigid, mostly solid interior. Thus, depending on the results from Juno\u2019s probing of Io\u2019s gravity field, we would be able to tell if a global magma ocean was hiding beneath its surface.<\/p>\n<\/blockquote>\n<p>The results suggested that Io does <em>not<\/em> have a global magma ocean. The deformation of Io\u2019s interior from the tidal flexing did not match what would be expected from a global layer of magma. Instead, each volcano is self-powered with its own localized pool of magma.<\/p>\n<p><iframe loading=\"lazy\" title=\"Animated Tour of Jupiter\u2019s Volcanic Moon Io\" width=\"1110\" height=\"624\" src=\"https:\/\/www.youtube.com\/embed\/Zpc_LCQD0hc?feature=oembed\" frameborder=\"0\" allow=\"accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture; web-share\" referrerpolicy=\"strict-origin-when-cross-origin\" allowfullscreen><\/iframe><br \/><em>Animated tour of Jupiter\u2019s volcanic moon Io. Video via NASA\/ JPL-Caltech\/ SwRI\/ Koji Kuramura\/ Gerald Eichst\u00e4dt.<\/em><\/p>\n<h3>Implications for other moons<\/h3>\n<p>Scientists can also apply the results to their studies of other moons. Instead of magma, some other moons in the outer solar system \u2013 such as Europa and Enceladus \u2013 have subsurface oceans. On both moons, those oceans are global. And on Enceladus \u2013 and maybe also Europa \u2013 there are huge geyser-like jets of water that erupt through the outer ice surface and into space. These are cryovolcanoes, which spew water, ice and ammonia (gas) instead of lava. Scientists can use the same techniques from Io in studying those moons as well, because they also experience tidal flexing. Lead author Ryan Park is a Juno co-investigator and supervisor of the Solar System Dynamics Group at JPL. He said:<\/p>\n<blockquote>\n<p>Juno\u2019s discovery that tidal forces do not always create global magma oceans does more than prompt us to rethink what we know about Io\u2019s interior. It has implications for our understanding of other moons, such as Enceladus and Europa, and even exoplanets and super-Earths. Our new findings provide an opportunity to rethink what we know about planetary formation and evolution.<\/p>\n<\/blockquote>\n<figure id=\"attachment_486658\" aria-describedby=\"caption-attachment-486658\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/earthsky.org\/upl\/2024\/09\/New-volcano-Io-April-2024-vs-Nov-1997-NASA-JPL-Caltech-SwRI-MSSS-Europlanet.jpg\" alt=\"A pockmarked moon in beige with dark spots, with an inset of a black-and-white area missing one of the pockmarks.\" width=\"650\" height=\"979\" class=\"size-full wp-image-486658\" srcset=\"https:\/\/earthsky.org\/upl\/2024\/09\/New-volcano-Io-April-2024-vs-Nov-1997-NASA-JPL-Caltech-SwRI-MSSS-Europlanet.jpg 650w, https:\/\/earthsky.org\/upl\/2024\/09\/New-volcano-Io-April-2024-vs-Nov-1997-NASA-JPL-Caltech-SwRI-MSSS-Europlanet-199x300.jpg 199w\" sizes=\"auto, (max-width: 650px) 100vw, 650px\"\/><figcaption id=\"caption-attachment-486658\" class=\"wp-caption-text\">View larger. | Here\u2019s an image of Jupiter\u2019s moon Io from February 2024. The black-and-white inset shows the same area from November 1997. You can see a new volcanic feature has formed in this area. Image via NASA\/ JPL-Caltech\/ SwRI\/ MSSS\/ Europlanet.<\/figcaption><\/figure>\n<h3>A new volcano!<\/h3>\n<p>Last September, scientists spotted a new volcano on Io, added to the hundreds it already has. They first saw it in Juno images from February 2024. And it\u2019s big, covering an area about 110 miles by 110 miles (180 km by 180 km) wide.<\/p>\n<p>Bottom line: Does Jupiter\u2019s moon Io have a global subsurface magma ocean? A new study said no, and that Io\u2019s raging volcanoes are self-powered with their own magma pools.<\/p>\n<p>Source: Io\u2019s tidal response precludes a shallow magma ocean<\/p>\n<p>Via NASA<\/p>\n<p>Read more: Jupiter\u2019s moon Io has a new volcano! See pics here<\/p>\n<p>Read more: Jupiter\u2019s moon Io as you\u2019ve never seen it<\/p>\n<p><span class=\"cp-load-after-post\"\/><\/div>\n<div>\n<div class=\"post-author\">\n<h4>Paul Scott Anderson<\/h4>\n<p>                    View Articles\n                  <\/p><\/div>\n<div class=\"post-tags\">\n<h6 data-udy-fe=\"text_7c58270d\">About the Author:<\/h6>\n<p>Paul Scott Anderson has had a passion for space exploration that began when he was a child when he watched Carl Sagan\u2019s Cosmos. He studied English, writing, art and computer\/publication design in high school and college. He later started his blog The Meridiani Journal in 2005, which was later renamed Planetaria. He also later started the blog Fermi Paradoxica, about the search for life elsewhere in the universe.&#13;<br \/>\n&#13;<br \/>\nWhile interested in all aspects of space exploration, his primary passion is planetary science and SETI. In 2011, he started writing about space on a freelance basis with Universe Today. He has also written for SpaceFlight Insider and AmericaSpace and has also been published in The Mars Quarterly. He also did some supplementary writing for the iOS app Exoplanet.&#13;<br \/>\n&#13;<br \/>\nHe has been writing for EarthSky since 2018, and also assists with proofing and social media.<\/p>\n<\/p><\/div>\n<\/p><\/div>\n<p><br \/>\n<br \/><a href=\"https:\/\/earthsky.org\/space\/ios-raging-volcanoes-magma-ocean-juno\/?rand=772280\">Source link <\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>View larger. | NASA\u2019s Juno spacecraft captured this view of Io on December 30, 2023. A new NASA study suggested Io doesn\u2019t have a global subsurface ocean of magma. Rather,&hellip; <\/p>\n","protected":false},"author":1,"featured_media":792272,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[46],"tags":[],"class_list":["post-792271","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-earth-sky"],"_links":{"self":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/792271","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=792271"}],"version-history":[{"count":0,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/792271\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/media\/792272"}],"wp:attachment":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=792271"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=792271"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=792271"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}