{"id":790713,"date":"2024-10-29T14:40:00","date_gmt":"2024-10-29T19:40:00","guid":{"rendered":"http:\/\/spaceweekly.com\/?p=790713"},"modified":"2024-10-29T14:40:00","modified_gmt":"2024-10-29T19:40:00","slug":"titan-may-have-a-methane-crust-10-km-thick","status":"publish","type":"post","link":"https:\/\/spaceweekly.com\/?p=790713","title":{"rendered":"Titan May Have a Methane Crust 10 Km Thick"},"content":{"rendered":"<p> <br \/>\n<\/p>\n<div>\n<p>Saturn\u2019s moon, Titan, is an anomaly among moons. No other moons have surface liquids, and aside from Earth, it\u2019s the only other Solar System object with liquids on its surface. However, since Titan is so cold, the liquids are hydrocarbons, not water. Titan\u2019s water is all frozen into a surface layer of ice.<\/p>\n<p>New research suggests that under the surface, Titan is hiding another anomaly: a thick crust of methane. <\/p>\n<p><span id=\"more-169048\"\/><\/p>\n<p>The evidence for the methane comes mostly from craters. Observations have found few confirmed impact craters on the frigid moon, and the ones that have been observed are hundreds of meters shallower than the same-sized craters on other moons. If Titan\u2019s crust was rock, the craters should be much deeper. <\/p>\n<p>The new research<span style=\"box-sizing: border-box; margin: 0px; padding: 0px;\">, published in The Planetary Science Journal, is titled \u201cRapid Impact Crater Relaxation Caused by an Insulating Methane Clathrate Crust on Titan.\u201d Lauren Schurmeier, from the Hawai\u2019i Institute of Geophysics and Planetology at the University of Hawai\u2019i at Manoa, is the lead author<\/span>. <\/p>\n<p>Titan stands apart from other moons for multiple reasons. Unlike any other natural satellites in the Solar System, it has a thick atmosphere. Its atmosphere is about 50% more dense than Earth\u2019s and extends about 600 km into space. A haze made of complex organic molecules called tholins gives the atmosphere its characteristic orange colour. The atmosphere is so thick that it blocks optical light, making Titan\u2019s surface features nearly inscrutable.<\/p>\n<p>The Cassini spacecraft has given us our best looks at Titan. It used radar and infrared instruments to see the moon\u2019s surface. The small Huygens probe that went to Saturn with Cassini was released into Titan in 2005 to study the atmosphere and surface. It\u2019s thanks to Huygens that we have our best images of Titan\u2019s surface.<\/p>\n<figure class=\"wp-block-embed is-type-video is-provider-youtube wp-block-embed-youtube wp-embed-aspect-16-9 wp-has-aspect-ratio\">\n<p>\n<span class=\"embed-youtube\" style=\"text-align:center; display: block;\"><iframe loading=\"lazy\" title=\"Titan Touchdown\" width=\"1110\" height=\"624\" src=\"https:\/\/www.youtube.com\/embed\/msiLWxDayuA?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><\/span>\n<\/p>\n<\/figure>\n<p>The new research suggests a link between Titan\u2019s unusual atmosphere, its shallow surface craters, and a layer of methane in the moon\u2019s crust. The methane keeps the underlying layer of ice convective by insulating it and helps impact craters rebound quickly and remain shallow.<\/p>\n<p>There\u2019s no consensus on how many craters Titan has because its surface is veiled behind its thick atmosphere, but there is some data on the craters.<\/p>\n<figure class=\"wp-block-image size-full\"><figcaption class=\"wp-element-caption\">This graph shows crater candidate counts binned by latitude regions and certainty level. Craters of certainty level 1 have more lines of evidence pointing toward an impact crater origin; certainty level 4 is the least certain. Image Credit: Schurmeier et al. 2024.<\/figcaption><\/figure>\n<p>The research centres on the fact that Titan displays few craters and that the ones we do see are shallow. This sets it apart from other moons.<\/p>\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"672\" height=\"700\" src=\"https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/10\/Low-Res_3-Titan-Craters-copy.jpg\" alt=\"These are Cassini SAR (synthetic aperture radar) images of Titan's impact craters. Arrows indicate potential forms of crater modification processes, including dunes and sands (purple), channels (blue), and significant crater rim erosion (pink). Afekan crater is one of Titan's largest impact craters at 115 km. Jupiter's moon, Ganymede, which is about the same size as Titan, has way more craters, including 20 that are much larger than Afekan. Image Credit: NASA\/ Cassini\" class=\"wp-image-169060\" srcset=\"https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/10\/Low-Res_3-Titan-Craters-copy.jpg 672w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/10\/Low-Res_3-Titan-Craters-copy-557x580.jpg 557w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/10\/Low-Res_3-Titan-Craters-copy-240x250.jpg 240w\" sizes=\"auto, (max-width: 672px) 100vw, 672px\"\/><figcaption class=\"wp-element-caption\">These are Cassini SAR (synthetic aperture radar) images of Titan\u2019s impact craters. Arrows indicate potential forms of crater modification processes, including dunes and sands (purple), channels (blue), and significant crater rim erosion (pink). Afekan crater is one of Titan\u2019s largest impact craters at 115 km. Jupiter\u2019s moon, Ganymede, which is about the same size as Titan, has way more craters, including 20 that are larger than Afekan. Image Credit: NASA\/ Cassini<\/figcaption><\/figure>\n<p>\u201cThis was very surprising because, based on other moons, we expect to see many more impact craters on the surface and craters that are much deeper than what we observe on Titan,\u201d said lead author Schurmeier. \u201cWe realized something unique to Titan must be making them become shallower and disappear relatively quickly.\u201d<\/p>\n<p>A handful of processes have been proposed to explain Titan\u2019s diminishing craters. Liquid hydrocarbon rainfall, aeolian sand infill, and topographic relaxation induced by insulating sand infill have all been discussed. \u201cHere, we propose an additional mechanism: topographic relaxation due to an insulating methane clathrate crustal layer in Titan\u2019s upper ice shell,\u201d the authors write.<\/p>\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"700\" height=\"526\" src=\"https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/10\/Low-Res_1-Titan-Interior_cropped.jpg\" alt=\"This simple schematic of Titan's interior (not to scale) shows a methane clathrate crust over a convecting ice shell.\u00a0The methane clathrate can insulate the ice below and keep it convective. That convection could explain why Titan's craters are so few and so shallow. Image Credit: Schurmeier et al. 2024.\" class=\"wp-image-169062\" srcset=\"https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/10\/Low-Res_1-Titan-Interior_cropped.jpg 700w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/10\/Low-Res_1-Titan-Interior_cropped-580x436.jpg 580w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/10\/Low-Res_1-Titan-Interior_cropped-250x188.jpg 250w\" sizes=\"auto, (max-width: 700px) 100vw, 700px\"\/><figcaption class=\"wp-element-caption\">This simple schematic of Titan\u2019s interior (not to scale) shows a methane clathrate crust over a convecting ice shell.\u00a0The methane clathrate can insulate the ice below and keep it convective. That convection could explain why Titan\u2019s craters are so few and so shallow. Image Credit: Schurmeier et al. 2024. <br \/>\u00a0<\/figcaption><\/figure>\n<p>There\u2019s very little new information coming from Titan, so researchers have to work with what they have. To try to understand its shallow craters, the researchers built a computer model. They used it to try to understand how Titan\u2019s topography might respond to impacts if a layer of methane clathrate was trapped under the surface. A clathrate is a substance where one type of molecule is trapped within a structure of molecules of another type. In this case, methane is trapped in water ice. <\/p>\n<p>Methane\u2019s insulating properties are key. <\/p>\n<p>\u201cMethane clathrate is stronger and more insulating than regular water ice,\u201d said Schurmeier. \u201cA clathrate crust insulates Titan\u2019s interior, makes the water ice shell very warm and ductile, and implies that Titan\u2019s ice shell is or was slowly connecting.\u201d<\/p>\n<p>With their model, they tested clathrate crusts that were 5, 10, 15, or 20 km thick. They used craters that were 40, 85, 100, and 120 km in diameter, each with two initial depths based on Ganymede\u2019s crater diameters and depths. The result?<\/p>\n<p>\u201cWe find that all clathrate crustal thicknesses result in rapid topographic relaxation despite Titan\u2019s cold surface temperature,\u201d the researchers write. \u201cThe 5 km thick clathrate crust can reproduce nearly all of the observed shallow depths, many in under 1000 yrs.\u201d <\/p>\n<p>They also found that a 10 km clathrate crust can reproduce Titan\u2019s observed crater depths over geologic timescales. \u201cIf relaxation is the primary cause of the shallow craters, then the clathrate thickness is likely 5\u201310 km thick,\u201d they write. <\/p>\n<p>Across all simulations, most of the crater relaxation occurred in 1,000 years. \u201cThis finding suggests that thin clathrate crusts cause crater shallowing in a geological instant, similar to a fast-flowing terrestrial glacier,\u201d the authors explain. It could certainly explain why none of Titan\u2019s craters are deep. <\/p>\n<p>The researchers point out a couple of caveats, though. They assumed that Titan\u2019s initial craters had depths similar to Ganymede\u2019s. They could\u2019ve formed at different depths and shapes. Their model also didn\u2019t include heat generated by the impact itself or account for an impact-triggered discontinuity in the methane clathrate layer. \u201cThese thermal and dynamic changes might alter the morphological evolution of the crater,\u201d they write.<\/p>\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"948\" src=\"https:\/\/www.universetoday.com\/wp-content\/uploads\/2023\/03\/Ganymede_-_Perijove_34_Composite-e1699297666973.jpg\" alt=\"Juno captured this image of Ganymede in July 2022. The moon's impact craters are easily visible, including the crater Tros, which is prominent below the center at left. Image Credit: NASA\/JPL-Caltech\/SwRI\/MSSS\/Kevin M. Gill\" class=\"wp-image-160666\" srcset=\"https:\/\/www.universetoday.com\/wp-content\/uploads\/2023\/03\/Ganymede_-_Perijove_34_Composite-e1699297666973.jpg 1024w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2023\/03\/Ganymede_-_Perijove_34_Composite-e1699297666973-580x537.jpg 580w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2023\/03\/Ganymede_-_Perijove_34_Composite-e1699297666973-250x231.jpg 250w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2023\/03\/Ganymede_-_Perijove_34_Composite-e1699297666973-768x711.jpg 768w\" sizes=\"auto, (max-width: 767px) 89vw, (max-width: 1000px) 54vw, (max-width: 1071px) 543px, 580px\"\/><figcaption class=\"wp-element-caption\">Juno captured this image of Ganymede in July 2022. The moon\u2019s impact craters are easily visible, including the crater Tros, which is prominent below the center at left. Image Credit: NASA\/JPL-Caltech\/SwRI\/MSSS\/Kevin M. Gill<\/figcaption><\/figure>\n<p>This research adds to Titan\u2019s mystery and our fascination with the unusual moon. It also adds another element to comparisons with Earth. Earth and Titan both have surface liquid and are the only two objects in the Solar System that do. Earth also has methane clathrates in its polar regions. <\/p>\n<p>\u201cTitan is a natural laboratory to study how the greenhouse gas methane warms and cycles through the atmosphere,\u201d said Schurmeier. \u201cEarth\u2019s methane clathrate hydrates, found in the permafrost of Siberia and below the arctic seafloor, are currently destabilizing and releasing methane. So, lessons from Titan can provide important insights into processes happening on Earth.\u201d <\/p>\n<p>In the end, their results are clear: \u201cWe conclude that if crater relaxation is the primary cause of Titan\u2019s unexpectedly shallow craters, then the clathrate crust is 5\u201310 km thick,\u201d the authors write. <\/p>\n<div class=\"sharedaddy sd-block sd-like jetpack-likes-widget-wrapper jetpack-likes-widget-unloaded\" id=\"like-post-wrapper-24000880-169048-67213792611a1\" data-src=\"https:\/\/widgets.wp.com\/likes\/?ver=13.2.3#blog_id=24000880&amp;post_id=169048&amp;origin=www.universetoday.com&amp;obj_id=24000880-169048-67213792611a1&amp;n=1\" data-name=\"like-post-frame-24000880-169048-67213792611a1\" data-title=\"Like or Reblog\">\n<h3 class=\"sd-title\">Like this:<\/h3>\n<p><span class=\"button\"><span>Like<\/span><\/span> <span class=\"loading\">Loading&#8230;<\/span><\/p>\n<p><span class=\"sd-text-color\"\/><\/div>\n<\/p><\/div>\n<p><br \/>\n<br \/><a href=\"https:\/\/www.universetoday.com\/169048\/titan-may-have-a-methane-crust-10-km-thick\/?rand=772204\">Source link <\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Saturn\u2019s moon, Titan, is an anomaly among moons. No other moons have surface liquids, and aside from Earth, it\u2019s the only other Solar System object with liquids on its surface.&hellip; <\/p>\n","protected":false},"author":1,"featured_media":790714,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[13],"tags":[],"class_list":["post-790713","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-genaero"],"_links":{"self":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/790713","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=790713"}],"version-history":[{"count":0,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/790713\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/media\/790714"}],"wp:attachment":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=790713"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=790713"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=790713"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}