{"id":787374,"date":"2024-08-16T05:25:50","date_gmt":"2024-08-16T10:25:50","guid":{"rendered":"https:\/\/spaceweekly.com\/?p=787374"},"modified":"2024-08-16T05:25:50","modified_gmt":"2024-08-16T10:25:50","slug":"asaph-hall-finds-mars-moon-phobos-147-years-ago","status":"publish","type":"post","link":"https:\/\/spaceweekly.com\/?p=787374","title":{"rendered":"Asaph Hall finds Mars moon Phobos 147 years ago"},"content":{"rendered":"<p> <br \/>\n<\/p>\n<div>\n<figure id=\"attachment_231026\" aria-describedby=\"caption-attachment-231026\" style=\"width: 800px\" class=\"wp-caption alignnone\"><figcaption id=\"caption-attachment-231026\" class=\"wp-caption-text\">Asaph Hall discovered Phobos on August 17, 1877. This image of the large crater Stickney on the Martian moon Phobos is color-enhanced. The crater is 5.6 miles (9 km) in diameter, so it covers a substantial proportion of Phobos\u2019 surface. The impact almost destroyed the small moon! Notice the smaller crater within Stickney, about 1.2 miles (2 km) in diameter, resulting from a later impact. Image via HiRISE\/ MRO\/ LPL (U. Arizona)\/ NASA.<\/figcaption><\/figure>\n<h3>August 17, 1877: Asaph Hall discovers Phobos<\/h3>\n<p>On August 17, 147 years ago, American astronomer Asaph Hall discovered the first known moon for our neighboring planet, Mars. Later that year, he found a second Martian moon. Today, we call the first and larger moon Phobos. And we call the second and smaller one Deimos. <\/p>\n<p>To date, Phobos and Deimos remain the only known moons of Mars.<\/p>\n<p>Both Phobos and Deimos are potato-shaped. They look more like asteroids than like Earth\u2019s much-larger companion moon. In fact, it\u2019s likely that Mars captured these little worlds that now orbit the red planet. Studies have indicated that \u2013 millions of years from now \u2013 Phobos will shatter and form a ring around Mars. Some astronomers think Phobos alternates between being a planetary ring, then clumping up again to form a moon. More about ring theories of Phobos below.<\/p>\n<h3>Phobos and Deimos, fear and terror<\/h3>\n<p>The names Phobos and Deimos mean <em>fear<\/em> and <em>terror<\/em>, respectively. They\u2019re named for the mythological horses that pulled the chariot of the Greek war god Ares. He was the Greek counterpart to the Roman war god Mars. <\/p>\n<p>So, although it\u2019s the larger of Mars\u2019 two moons, Phobos is tiny. It has a mean diameter of only about 14 miles (22.2 km). But it\u2019s seven times more massive than Deimos, which has a mean diameter of about 7.7 miles (12.4 km). For these moons, we\u2019re speaking in terms of a mean diameter because both moons are oblong in shape and not spherical. In contrast, Earth\u2019s moon is nearly round, since it\u2019s large enough for its gravity to have pulled it into a spherical shape. <\/p>\n<p>Earth\u2019s moon is also much larger (2,159 miles or 3,475 km in diameter). Since both Phobos and Deimos are so tiny, they have very weak gravity. And that means they don\u2019t have enough gravity to make them round.<\/p>\n<h3>Mariner 9 was 1st to see them close<\/h3>\n<p>During Mariner 9\u2019s mission to Mars in 1971 and 1972, scientists got their first close-up look at Phobos. Just like asteroids, its oblong surface shows many small craters. But one large crater stood out as much bigger than the rest. Astronomers named it Stickney Crater, for Angeline Stickney \u2013 an an American academic, suffragist and mathematician \u2013 and Asaph Hall\u2019s wife. <\/p>\n<p>Stickney looks like a giant hole on one end of Phobos. Whatever rocky body created it was almost big enough to have shattered the moon. It\u2019s thought that, whenever the impact occurred, Phobos barely survived.<\/p>\n<figure id=\"attachment_179711\" aria-describedby=\"caption-attachment-179711\" style=\"width: 800px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-179711\" src=\"https:\/\/earthsky.org\/upl\/2013\/08\/phobos-stickney-crater-e1376739889102.png\" alt=\"Oval object half in shadow with giant dent in one end.\" width=\"800\" height=\"749\"\/><figcaption id=\"caption-attachment-179711\" class=\"wp-caption-text\">Viking I image of Phobos and its large crater Stickney. The spacecraft captured this image in June 1977, 100 years after the discovery of Phobos. Image via NASA\/ ESA.<\/figcaption><\/figure>\n<figure id=\"attachment_342364\" aria-describedby=\"caption-attachment-342364\" style=\"width: 800px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-342364\" src=\"https:\/\/earthsky.org\/upl\/2018\/08\/Phobos-Mars-Nov-28-2018.jpg\" alt=\"Oblong rocky moon covered with craters and straight grooves, in black space.\" width=\"800\" height=\"790\" srcset=\"https:\/\/earthsky.org\/upl\/2018\/08\/Phobos-Mars-Nov-28-2018.jpg 580w, https:\/\/earthsky.org\/upl\/2018\/08\/Phobos-Mars-Nov-28-2018-300x296.jpg 300w, https:\/\/earthsky.org\/upl\/2018\/08\/Phobos-Mars-Nov-28-2018-190x188.jpg 190w, https:\/\/earthsky.org\/upl\/2018\/08\/Phobos-Mars-Nov-28-2018-140x138.jpg 140w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\"\/><figcaption id=\"caption-attachment-342364\" class=\"wp-caption-text\">A closer view of the grooves on Phobos. Image via NASA\/ JPL-Caltech\/ University of Arizona.<\/figcaption><\/figure>\n<figure id=\"attachment_342366\" aria-describedby=\"caption-attachment-342366\" style=\"width: 800px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-342366 size-large\" src=\"https:\/\/earthsky.org\/upl\/2018\/08\/Phobos-Viking-global-map-Nov-28-2018-800x400.jpg\" alt=\"Gray terrain covered by craters and grooves.\" width=\"800\" height=\"400\"\/><figcaption id=\"caption-attachment-342366\" class=\"wp-caption-text\">The Viking orbiter obtained this global map of Phobos. Image via Astrogeology Science Center\/ Planetary Data System\/ Phil Stooke.<\/figcaption><\/figure>\n<h3>Was Phobos once a ring? Will it be again?<\/h3>\n<p>Phobos has long, shallow grooves running across its surface, radiating away from Stickney. Many planetary scientists believe these grooves are early signs of eventual structural failure in the moon. They say it\u2019s possible that \u2013 some 50 million years from now \u2013 Phobos will break apart, forming a ring around Mars.<\/p>\n<p>A study in 2018 suggested that rolling boulders created the grooves, spraying across the surface during impact. As Ken Ramsley, a planetary science researcher at Brown University who led the work, explained:<\/p>\n<blockquote>\n<p>These grooves are a distinctive feature of Phobos, and planetary scientists have been debating how they formed for 40 years. We think this study is another step toward zeroing in on an explanation.<\/p>\n<\/blockquote>\n<h3>More ring theories<\/h3>\n<p>In 2017, a new theory by Purdue University scientists suggested Phobos might not only break apart and form a ring around the planet but also suggests this ring formation happened before.<\/p>\n<p>David Minton, a professor, and Andrew Hesselbrock, a doctoral student, both at Purdue, developed a computer model showing debris ejected into space from an asteroid or other body slamming into Mars. This event \u2013 some 4.3 billion years ago \u2013 would cause the material to now alternate between becoming a planetary ring and clumping up again to form the moon Phobos.<\/p>\n<figure id=\"attachment_342471\" aria-describedby=\"caption-attachment-342471\" style=\"width: 800px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-342471 size-large\" src=\"https:\/\/earthsky.org\/upl\/2020\/08\/Phobos-Deimos-comparison-NASA-800x377.jpg\" alt=\"2 rocky objects, 1 twice the apparent size of the other, next to each other on black background with stars.\" width=\"800\" height=\"377\"\/><figcaption id=\"caption-attachment-342471\" class=\"wp-caption-text\">Size and visual comparison of Phobos (left) and Deimos (right). Image via NASA.<\/figcaption><\/figure>\n<blockquote class=\"twitter-tweet\">\n<p lang=\"en\" dir=\"ltr\">Daily Owl <a rel=\"nofollow\" href=\"https:\/\/twitter.com\/hashtag\/Fact?src=hash&amp;ref_src=twsrc%5Etfw\">#Fact<\/a> <\/p>\n<p>One day <a rel=\"nofollow\" href=\"https:\/\/twitter.com\/hashtag\/Mars?src=hash&amp;ref_src=twsrc%5Etfw\">#Mars<\/a> will have a ring around it?<\/p>\n<p>In the next 20-40 million years Mars\u2019 largest moon Phobos will be torn apart by gravitational forces leading to the creation of a ring that could last up to 100 million years<a rel=\"nofollow\" href=\"https:\/\/twitter.com\/hashtag\/NFTs?src=hash&amp;ref_src=twsrc%5Etfw\">#NFTs<\/a> <a rel=\"nofollow\" href=\"https:\/\/twitter.com\/hashtag\/Moon?src=hash&amp;ref_src=twsrc%5Etfw\">#Moon<\/a> <a rel=\"nofollow\" href=\"https:\/\/twitter.com\/hashtag\/Space?src=hash&amp;ref_src=twsrc%5Etfw\">#Space<\/a> <a rel=\"nofollow\" href=\"https:\/\/t.co\/IIYHCkgDhf\">pic.twitter.com\/IIYHCkgDhf<\/a><\/p>\n<p>\u2014 MarsBirds? (@mars_birds) <a rel=\"nofollow\" href=\"https:\/\/twitter.com\/mars_birds\/status\/1546691566835666944?ref_src=twsrc%5Etfw\">July 12, 2022<\/a><\/p>\n<\/blockquote>\n<h3>Deimos played a role<\/h3>\n<p>Another study, from scientists at Purdue and the SETI Institute in June 2020, also concluded that Mars used to have a ring or series of rings. The scientists based that study on an analysis of the orbit of the other Martian moon, Deimos. <\/p>\n<p>Deimos is smaller than Phobos. And it has an orbit that\u2019s tilted with respect to Mars\u2019 equator by about 2 degrees. Meanwhile, Phobos\u2019 orbit isn\u2019t inclined as much. The larger moon is inclined to Mars\u2019 equator by only about 1 degree. The scientists said in a statement:<\/p>\n<blockquote>\n<p>These orbital resonances are picky but predictable \u2026 We can tell that only an outward-moving moon could have strongly affected Deimos, which means that Mars must have had a ring pushing the inner moon outward \u2026 This moon may have been 20 times as massive as Phobos, and may have been its \u2018grandparent\u2019 existing just over 3 billion years ago \u2026 [It] was followed by two more ring-moon cycles, with the latest moon being Phobos.<\/p>\n<\/blockquote>\n<p>So, basically, there may have been a moon about 20 times more massive than Phobos, and Mars\u2019 rings pushed it outward. And at least two times since then, that moon broke apart and then formed a new ring, before the material coalesced together again to form a new moon. Phobos is now that current moon.The scientists say it will eventually break apart to form a new ring, thus continuing the cycle.<\/p>\n<p>Scientists also now know Phobos is much younger than Deimos \u2013 perhaps only 200 million years old \u2013 which would fit the moon\/ring scenario. The Phobos we see today is simply a newer and smaller version of its original self.<\/p>\n<h3>Eclipsing moons<\/h3>\n<p>Asaph Hall probably never imagined the idea of Phobos breaking apart and forming a ring around Mars. And he couldn\u2019t possibly have imagined the video below, which was acquired by NASA\u2019s Mars rover Curiosity on August 1, 2013. This video shows both moons, Phobos and Deimos, as you might see them while standing on the surface of Mars. You can clearly see some of the large craters on Phobos in these images.<\/p>\n<p>This was the first time that images taken from Mars\u2019 surface caught one moon eclipsing the other \u2026 but probably not the last.<\/p>\n<p><iframe loading=\"lazy\" title=\"Two Moons Passing in the Martian Night\" width=\"1110\" height=\"624\" src=\"https:\/\/www.youtube.com\/embed\/DaVSCmuOJwI?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 data-mce-type=\"bookmark\" style=\"display: inline-block; width: 0px; overflow: hidden; line-height: 0;\" class=\"mce_SELRES_start\">?<\/span><\/iframe><\/p>\n<p>Bottom line: On August 17, 1877, American astronomer Asaph Hall discovered Phobos, the larger of the two Martian moons. He discovered Deimos later that year.<\/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. While in school he was known for his passion for space exploration and astronomy. He started his blog The Meridiani Journal in 2005, which was a chronicle of planetary exploration. In 2015, the blog was renamed as Planetaria. While interested in all aspects of space exploration, his primary passion is planetary science. In 2011, he started writing about space on a freelance basis, and now currently writes for AmericaSpace and Futurism (part of Vocal). He has also written for Universe Today and SpaceFlight Insider, and has also been published in The Mars Quarterly and has done supplementary writing for the well-known iOS app Exoplanet for iPhone and iPad.<\/p>\n<\/p><\/div>\n<\/p><\/div>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><br \/>\n<br \/><br \/>\n<br \/><a href=\"https:\/\/earthsky.org\/space\/this-date-in-science-asaph-hall-discovers-a-moon-for-mars\/?rand=772280\">Source link <\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Asaph Hall discovered Phobos on August 17, 1877. This image of the large crater Stickney on the Martian moon Phobos is color-enhanced. The crater is 5.6 miles (9 km) in&hellip; <\/p>\n","protected":false},"author":1,"featured_media":787375,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[46],"tags":[],"class_list":["post-787374","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\/787374","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=787374"}],"version-history":[{"count":0,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/787374\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/media\/787375"}],"wp:attachment":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=787374"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=787374"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=787374"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}