{"id":14746,"date":"2024-01-28T12:54:35","date_gmt":"2024-01-28T12:54:35","guid":{"rendered":"https:\/\/shareperformanceinsight.com\/index.php\/2024\/01\/28\/what-you-should-know-about-the-moon-area-where-japans-lander-touched-down\/"},"modified":"2024-01-28T12:54:35","modified_gmt":"2024-01-28T12:54:35","slug":"what-you-should-know-about-the-moon-area-where-japans-lander-touched-down","status":"publish","type":"post","link":"https:\/\/shareperformanceinsight.com\/index.php\/2024\/01\/28\/what-you-should-know-about-the-moon-area-where-japans-lander-touched-down\/","title":{"rendered":"What you should know about the moon area where Japan\u2019s lander touched down"},"content":{"rendered":"<div>\n<p class=\"paragraph inline-placeholder\">      The journey of \u201cMoon Sniper,\u201d the robotic explorer that has made Japan only the fifth country to put a spacecraft safely on the lunar surface, hasn\u2019t gone quite as expected.  <\/p>\n<p class=\"paragraph inline-placeholder\">      Though the mission \u2014 officially known as the Smart Lander for Investigating Moon, or SLIM \u2014 reached its destination last week, an \u201canomaly\u201d experienced during descent resulted in the vehicle landing with its solar panels facing the wrong direction, forcing it to operate on limited battery power, according to the Japan Aerospace Exploration Agency.  <\/p>\n<div class=\"related-content_full-width related-content_full-width--article\">\n<div class=\"related-content_full-width__image image__related-content\">            <\/div>\n<p class=\"related-content_full-width__headline\">            <span class=\"related-content_full-width__title-text\"><\/span>      <span class=\"related-content_full-width__headline-text\">The moon has entered a new epoch, scientists say<\/span>    <\/p>\n<\/div>\n<p class=\"paragraph inline-placeholder\">      Now, with Moon Sniper\u2019s battery turned off to maintain spacecraft functionality, JAXA officials are in wait-and-see mode, hoping the changing angle of the sun will restore power to the vehicle and allow the mission to resume. If the lander turns on again, it could make good on its objectives to collect unprecedented information about a region called the Sea of Nectar.  <\/p>\n<p class=\"paragraph inline-placeholder\">      The spacecraft touched down near \ufeffa crater called Shioli \u2014 a Japanese female first name pronounced \u201cshe-oh-lee\u201d \u2014 which sits about 200 miles (322 kilometers) south of the Sea of Tranquility, the region near the lunar equator where Apollo 11 first landed humans on the moon.  <\/p>\n<p class=\"paragraph inline-placeholder\">      At around 880 feet (268 meters) in diameter, it\u2019s a small crater, but it\u2019s close to a much bigger one called Theophilus that\u2019s more than 60 miles (97 kilometers) across. This detail makes it particularly interesting for exploration.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cWhen I was reading up about this a month or so ago, I was super excited to see they had chosen this site,\u201d said Dr. Gordon Osinski, a professor of planetary geology at Western University in Ontario, who\u2019s also part of the upcoming Artemis III moon mission\u2019s geology team.  <\/p>\n<div class=\"related-content_full-width related-content_full-width--article\">\n<div class=\"related-content_full-width__image image__related-content\">            <\/div>\n<p class=\"related-content_full-width__headline\">            <span class=\"related-content_full-width__title-text\"><\/span>      <span class=\"related-content_full-width__headline-text\">NASA delays astronaut moon landing to at least 2026<\/span>    <\/p>\n<\/div>\n<p class=\"paragraph inline-placeholder\">      \u201cOne of the great things about craters is that they excavate rocks from the depth and essentially give us a window into what\u2019s under the surface of a planetary body,\u201d Osinski added. He noted that Shioli stands on ground ejected by the larger nearby crater, which probably comes from a depth of over 1 mile (1.6 kilometers), giving researchers a chance to study lunar rock without any drilling.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cI think they chose this particular crater because the mineral olivine has been found \u2014 and anytime you mention olivine, people\u2019s eyes light up because we think it probably originates from the mantle of the moon, which we\u2019ve never really sampled on site before,\u201d Osinski said.  <\/p>\n<h3 class=\"subheader\">    Space weathering<\/h3>\n<p class=\"paragraph inline-placeholder\">      In November, NASA published photographs of Shioli taken by the Lunar Reconnaissance Orbiter, a spacecraft currently orbiting the moon and mapping it to aid future missions. In the black-and-white photo, the crater looks like a splotch of light.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cThe moon doesn\u2019t have an atmosphere like the Earth, so it isn\u2019t protected and it\u2019s constantly bombarded with micrometeorites and radiation that damage the surface layers,\u201d said Sara Russell, a professor of planetary sciences and senior research lead at the Planetary Materials Group of London\u2019s Natural History Museum.  <\/p>\n<p class=\"paragraph inline-placeholder\">      The crater is lighter in color because radiation and micrometeorites haven\u2019t had enough time to darken it yet: \u201cWhen a crater happens, it throws up material that was buried and that might be more pristine, because it hasn\u2019t experienced this damage, which we call space weathering. It gives us fresh rock to look at that, and potentially learn more about the moon,\u201d she said.  <\/p>\n<p class=\"paragraph inline-placeholder\">      Opportunities to study these rare rock samples make the moon a brilliant geology laboratory, Russell added.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cWhatever the moon has experienced, the Earth has also experienced. Looking at craters can also tell us something about the Earth\u2019s own history, because rocks form there without any of the complicating factors that we have on Earth, like water and life and the wind,\u201d she said. \u201cIt\u2019s a beautiful experiment in the sky.\u201d  <\/p>\n<p class=\"paragraph inline-placeholder\">      After landing in the crater, the spacecraft captured 257 low-resolution images of its surroundings, and the mission team later gave nicknames to some of the rocks in the pictures. More images will be taken if the lander manages to regain power.  <\/p>\n<h3 class=\"subheader\">    Pinpoint accuracy<\/h3>\n<p class=\"paragraph inline-placeholder\">      Another reason for choosing the vicinity of Shioli as the landing site for Japan\u2019s SLIM mission is that its small size was an ideal training ground for the lander\u2019s pinpoint accuracy, which allowed it to target an area spanning just 328 feet (100 meters) across for touchdown. Living up to its nickname, the Moon Sniper actually landed just 180 feet (55 meters) shy of its target, which JAXA deemed a \u201csignificant achievement.\u201d  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cThey\u2019re really using the technology to show that they can land in very small landing circles, which would be quite a step forward for capabilities to land on different planets,\u201d said Dr. John Pernet-Fisher, a research fellow in geochemistry and cosmochemistry at the University of Manchester in the United Kingdom, in an interview before the landing.  <\/p>\n<p class=\"paragraph inline-placeholder\">      Traditionally, moon missions target areas a few kilometers wide for touchdown: \u201cBut that really limits where you can land, because you have to make sure that within the whole landing area every point it is safe to land on,\u201d he added. \u201cThat makes things a lot more difficult if you want to land in more challenging or rugged terrain, so this can really open the doors to being able to land in areas that are topographically a bit more varied and therefore might tell us something different about the moon and its formation.\u201d  <\/p>\n<div class=\"related-content_full-width related-content_full-width--article\">\n<div class=\"related-content_full-width__image image__related-content\">            <\/div>\n<p class=\"related-content_full-width__headline\">            <span class=\"related-content_full-width__title-text\"><\/span>      <span class=\"related-content_full-width__headline-text\">Apollo 17 astronauts collected rocks that reveal the moon\u2019s true age<\/span>    <\/p>\n<\/div>\n<p class=\"paragraph inline-placeholder\">      The Moon Sniper\u2019s landing site is not far from the point where Apollo 16 touched down in 1972. That older mission\u2019s crew collected 731 individual rock and soil samples for a total mass of 95.7 kilograms (210 pounds), according to the Lunar and Planetary Institute. That\u2019s a sizable chunk of the 382 kilograms (842 pounds) that NASA brought back from the moon during the entire program.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cIf you think about it, we\u2019re trying to interpret the geological history of this whole body based on a collection of rocks from quite a geographically small area,\u201d Pernet-Fisher said. \u201cAnd so it\u2019s really important for us to gather as much data as possible from a huge diversity of different geographic locations. Even though this is still relatively near some of the Apollo missions, it\u2019s really important data that we\u2019ll be gathering.\u201d  <\/p>\n<h3 class=\"subheader\">    A sea of lava<\/h3>\n<p class=\"paragraph inline-placeholder\">      The largest lunar feature in the vicinity of Shioli is the Sea of Nectar, a basin 210 miles (339 kilometers) in diameter that is one of the oldest on the near side of the moon, the hemisphere that always faces Earth. The lunar plain is visible with binoculars or a small telescope, and was formed when the moon\u2019s surface was created about 3.9 billion years ago.  <\/p>\n<p class=\"paragraph inline-placeholder\">      The Sea of Nectar is much smaller than its neighbor the Sea of Tranquility, which is over 540 miles (875 kilometers) across and is similarly smooth and flat.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cTranquillity was chosen for the Apollo 11 landing not for any scientific reasons, but because it was one of the flattest, smoothest parts for the moon and therefore considered safest to land on,\u201d Western University\u2019s Osinski said.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cThat is also applicable for most robotic missions,\u201d he added. \u201cI\u2019m the principal investigator for Canada\u2019s first ever moon rover and we\u2019re looking at landing sites now. We\u2019re being driven towards smooth areas, away from craters or boulders, which actually may sound less scientifically interesting.\u201d  <\/p>\n<p class=\"paragraph inline-placeholder\">      The reason scientists call these basins \u201cseas,\u201d or \u201cmaria\u201d in the original Latin, is that ancient astronomers who first looked up at the moon believed they were filled with water, due to the darker hue.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cAfter the Apollo missions, we brought back samples and learned they were essentially massive lava planes,\u201d Osinski said. \u201cIt\u2019s not like there was a massive volcano with lava pouring out, but rather fissure eruptions, so the lava was just literally coming up through fractures. We can think of them as lava seas.\u201d  <\/p>\n<div class=\"related-content_full-width related-content_full-width--article\">\n<div class=\"related-content_full-width__image image__related-content\">            <\/div>\n<p class=\"related-content_full-width__headline\">            <span class=\"related-content_full-width__title-text\"><\/span>      <span class=\"related-content_full-width__headline-text\">Here\u2019s what India\u2019s historic lunar lander found on the moon \u2014 and what\u2019s next<\/span>    <\/p>\n<\/div>\n<p class=\"paragraph inline-placeholder\">      Water does come into play when looking at another area of the moon that will be targeted by upcoming landings, including NASA\u2019s first crewed Artemis mission, expected as soon as 2026: \u201cThe south polar region,\u201d Osinski said, \u201can area that is geologically interesting, and also rich with what we call volatiles \u2014 think water ice but also frozen carbon dioxide or ammonia.\u201d  <\/p>\n<p class=\"paragraph inline-placeholder\">      If humans can find a good, sizable source of water ice in the moon\u2019s south pole region and it\u2019s possible to extract it, the result could be a game changer for lunar exploration, according to Osinski.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cWe\u2019d have water for the astronauts to drink, we can extract the oxygen, and it can be broken down to get the hydrogen for rocket fuel. It also reduces costs, because water is one of the most expensive things to launch from Earth because it\u2019s so heavy,\u201d he said.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cIf we want to build lunar bases, which we all hope we do, we are going to have to find a source of water to use on the moon.\u201d  <\/p>\n\n<div>This post appeared first on cnn.com<\/div>\n<\/div>","protected":false},"excerpt":{"rendered":"<p>The journey of \u201cMoon Sniper,\u201d the robotic explorer that has made Japan only the fifth country to put a spacecraft safely on the lunar surface, hasn\u2019t gone quite as expected. Though the mission \u2014 officially known as the Smart Lander for Investigating Moon, or SLIM \u2014 reached its destination last week, an \u201canomaly\u201d experienced during <\/p>\n","protected":false},"author":0,"featured_media":14747,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[23],"tags":[],"class_list":{"0":"post-14746","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","7":"category-world"},"_links":{"self":[{"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/posts\/14746","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/types\/post"}],"replies":[{"embeddable":true,"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/comments?post=14746"}],"version-history":[{"count":0,"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/posts\/14746\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/media\/14747"}],"wp:attachment":[{"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/media?parent=14746"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/categories?post=14746"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/tags?post=14746"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}