{"id":802740,"date":"2026-06-21T06:49:34","date_gmt":"2026-06-21T11:49:34","guid":{"rendered":"https:\/\/spaceweekly.com\/?p=802740"},"modified":"2026-06-21T06:49:34","modified_gmt":"2026-06-21T11:49:34","slug":"artemis-missions-target-south-pole-aitken-basin-on-the-moon","status":"publish","type":"post","link":"https:\/\/spaceweekly.com\/?p=802740","title":{"rendered":"Artemis missions target South Pole\u2013Aitken basin on the moon"},"content":{"rendered":"<p> <br \/>\n<\/p>\n<div>\n<figure id=\"attachment_549657\" aria-describedby=\"caption-attachment-549657\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><figcaption id=\"caption-attachment-549657\" class=\"wp-caption-text\">View larger. | This globe map shows the South Pole-Aitken basin (blue) and surrounding regions. Here we see rocks from the moon\u2019s mantle, the thick, rocky layer directly beneath its thin outer crust. The rocks were blasted onto the surface by the giant impact that created this huge moon basin. Image via NASA\/ JPL-Caltech\/ Goddard\/ Gabe Gowman-U. Arizona\/ SwRI. Data from NASA\u2019s GRAIL mission and NASA\u2019s Lunar Reconnaissance Orbiter Laser Altimeter.<\/figcaption><\/figure>\n<ul>\n<li><strong>The South Pole-Aitken basin<\/strong> is the largest impact basin on the moon. It\u2019s on the moon\u2019s far side. How did it form?<\/li>\n<li><strong>Two new studies<\/strong> show that the asteroid that struck the moon, forming the basin, came from the north at a low angle. Rocks from both the lunar crust and mantle were ejected onto the surface.<\/li>\n<li><strong>Future Artemis astronauts<\/strong> will land in and around the South Pole-Aitken region. The new studies help show what the astronauts can expect to find.<\/li>\n<\/ul>\n<p><strong>You deserve a daily dose of good news.<\/strong> For the latest in science and the night sky, click here to subscribe to our free daily newsletter.<\/p>\n<h3>The South Pole\u2013Aitken basin region is a future landing site<\/h3>\n<p>When Artemis astronauts return to the moon in the near future, they\u2019ll land near the lunar south pole. Of the nine possible landing sites, some are within the South Pole-Aitken basin. Others are on or near the rim of the basin, while still others are just outside of it.<\/p>\n<p>For example, the sites Nobile Rim 1, Nobile Rim 2 and Haworth are within the basin (see map below). Malapert Massif is near the basin\u2019s rim. And de Gerlache Rim 2 is outside of the basin. Note that the basin\u2019s boundary is rather obscure and not sharply delineated. So it\u2019s not always clear which proposed landing sites are, technically, within the basin. <\/p>\n<p>Now researchers have published two new peer-reviewed papers about the South Pole-Aitken basin. One is in Science Advances (May 6, 2026). And the other is in JGR Planets (April 23, 2026).<\/p>\n<figure id=\"attachment_549826\" aria-describedby=\"caption-attachment-549826\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/earthsky.org\/upl\/2026\/06\/Artemis-landing-region-candidates-moon.jpg\" alt=\"Black and white image of cratered terrain seen from above, with 9 labeled yellow squares scattered around.\" width=\"800\" height=\"618\" class=\"size-full wp-image-549826\" srcset=\"https:\/\/earthsky.org\/upl\/2026\/06\/Artemis-landing-region-candidates-moon.jpg 800w, https:\/\/earthsky.org\/upl\/2026\/06\/Artemis-landing-region-candidates-moon-300x232.jpg 300w, https:\/\/earthsky.org\/upl\/2026\/06\/Artemis-landing-region-candidates-moon-768x593.jpg 768w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\"\/><figcaption id=\"caption-attachment-549826\" class=\"wp-caption-text\">View larger. | The 9 possible landing sites for future Artemis missions, in and around the South Pole-Aitken basin. Note that it will no longer be the Artemis 3 mission, in late 2027, that lands first. That mission will remain in Earth orbit. It will now be Artemis 4 and beyond for the landings. Image via NASA.<\/figcaption><\/figure>\n<h3>Water ice and sunlight<\/h3>\n<p>Here are two reasons this region was chosen for the astronauts: water ice and sunlight. The landing sites closest to the moon\u2019s south pole offer access to water ice, which the astronauts will need as a primary resource. The sites also experience long periods of sunlight.<\/p>\n<p>This giant moon basin is the moon\u2019s oldest and largest impact crater, on the far side of the moon. But how much do we really know about this region? On June 15, 2026, researchers at the Southwest Research Institute (SwRI) in California, said that they have found new details about the South Pole-Aitken basin.<\/p>\n<p>Since it is one of the oldest structures on the moon, the basin provides clues about the early solar system.<\/p>\n<p>William Bottke is the director of the Center for Lunar Origin and Evolution (CLOE) and executive director of SwRI\u2019s Science Directorate in Boulder, Colorado. He is also a co-author of both of the new studies. He said:<\/p>\n<blockquote>\n<p>The basin offers scientists a rare opportunity to study the moon\u2019s earliest history. The collision struck the lunar surface with such force that it may have excavated material from deep inside the moon, including portions of the lunar mantle [the region just below the moon\u2019s thin crust].<\/p>\n<\/blockquote>\n<p><iframe loading=\"lazy\" src=\"https:\/\/www.facebook.com\/plugins\/post.php?href=https%3A%2F%2Fwww.facebook.com%2Fsouthwestresearch%2Fposts%2Fpfbid0PvSKfY2kHbMToBgf1KuevVL2kiu5pmVUwnqMvsZFXW2DRpq9LPVbnB7ACBYhmUjzl&amp;show_text=true&amp;width=500\" width=\"500\" height=\"634\" style=\"border:none;overflow:hidden\" scrolling=\"no\" frameborder=\"0\" allowfullscreen=\"true\" allow=\"autoplay; clipboard-write; encrypted-media; picture-in-picture; web-share\"><\/iframe><\/p>\n<h3>Recreating the impact<\/h3>\n<p>To find out more about the future landing location for the Artemis astronauts, the researchers used advanced computer simulations and computer models. They recreated the impact that formed the basin. They found that the impacting asteroid came from the north and hit the moon\u2019s surface at a low angle. That\u2019s why the basin is more elongated in shape than round. (However, scientists said in 2024 that it\u2019s actually  slightly rounder than first thought). Shigeru Wakita at Purdue University, lead author of the South-Pole Aitken basin impact study, said:<\/p>\n<blockquote>\n<p>Our simulation produces the right shape and nature of the impact basin. It also tells us about the projectile that created it and the direction of the impact.<\/p>\n<\/blockquote>\n<p>Notably, the analysis suggests that the object that impacted was not just a simple asteroid. The impacting object must have been more complex, with an inner core surrounded by rock. The object\u2019s interior appears to have been <em>differentiated<\/em>, separated into distinct compositional layers, more like a small protoplanet than a plain rock. Protoplanets are like \u201cbaby planets,\u201d smaller objects forming from the accumulation of material in the early solar system. Many would eventually grow to become actual planets, like our own Earth.<\/p>\n<p>When the impactor hit the moon, it created a deep, uneven cavity. The rock in the middle of the basin melted, and material from both the moon\u2019s mantle and crust were thrown out into space.<\/p>\n<figure id=\"attachment_547360\" aria-describedby=\"caption-attachment-547360\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/earthsky.org\/upl\/2026\/05\/Aitken-basin-moon-south-pole-Artemis-2-e1779877233904.jpg\" alt=\"A piece of the lunar surface, seen from orbit, showing heavily cratered terrain.\" width=\"800\" height=\"533\" class=\"size-full wp-image-547360\"\/><figcaption id=\"caption-attachment-547360\" class=\"wp-caption-text\">Captured by the Artemis 2 crew, the heavily cratered eastern edge of the South Pole-Aitken basin \u2013 the moon\u2019s oldest and largest impact basin \u2013 offers a glimpse into billions of years of lunar geologic history. Image via NASA.<\/figcaption><\/figure>\n<figure id=\"attachment_315340\" aria-describedby=\"caption-attachment-315340\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/earthsky.org\/upl\/2019\/06\/South-Pole\u2013Aitken-basin-moon-Nov-5-2015-e1560468914300.png\" alt=\"Far side of the moon. Light gray and cratered, but without large dark blotches. Red circle around a large area.\" width=\"800\" height=\"800\" class=\"size-full wp-image-315340\"\/><figcaption id=\"caption-attachment-315340\" class=\"wp-caption-text\">The South Pole-Aitken basin (outlined) on the far side of the moon. Image via NASA\/ Sneeuwschaap\/ Wikimedia Commons.<\/figcaption><\/figure>\n<h3>Ejecta in the basin<\/h3>\n<p>The researchers also wanted to know how the ejecta from the impact was distributed in and around the basin. To do this, they compared high-resolution gravity data with models that include both crustal and mantle material. The result was that the basin likely contains a substantial amount of rock from the moon\u2019s mantle. Those rocks are also mixed into the ejecta blanket \u2013 the rocky debris \u2013 surrounding the basin.<\/p>\n<p>Also, there were smaller secondary impacts that brought some of those rocks to the surface. That is treasure for the future Artemis astronauts who will land there. Gabriel Gowman at the University of Arizona, lead author of the gravity-based study, said:<\/p>\n<blockquote>\n<p>The precise distribution of mantle material has been a big unknown. Our models indicate that the [South-Pole Aitken basin] impact ejected enough deep material to form a significant deposit that should still be accessible today. Most importantly, some of that material at a trace level may exist in regions being considered for the Artemis landings.<\/p>\n<\/blockquote>\n<figure id=\"attachment_549762\" aria-describedby=\"caption-attachment-549762\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/earthsky.org\/upl\/2026\/06\/Shigeru-Wakita-Purdue-University.jpeg\" alt=\"Smiling young man with short black hair wearing a sweater.\" width=\"800\" height=\"800\" class=\"size-full wp-image-549762\" srcset=\"https:\/\/earthsky.org\/upl\/2026\/06\/Shigeru-Wakita-Purdue-University.jpeg 800w, https:\/\/earthsky.org\/upl\/2026\/06\/Shigeru-Wakita-Purdue-University-300x300.jpeg 300w, https:\/\/earthsky.org\/upl\/2026\/06\/Shigeru-Wakita-Purdue-University-150x150.jpeg 150w, https:\/\/earthsky.org\/upl\/2026\/06\/Shigeru-Wakita-Purdue-University-768x768.jpeg 768w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\"\/><figcaption id=\"caption-attachment-549762\" class=\"wp-caption-text\">Shigeru Wakita at Purdue University is the lead author of the South-Pole Aitken basin impact paper. Image via Google Scholar.<\/figcaption><\/figure>\n<figure id=\"attachment_549763\" aria-describedby=\"caption-attachment-549763\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/earthsky.org\/upl\/2026\/06\/Gabriel-Gowman-University-of-Arizona.jpg\" alt=\"Smiling young man with longish, tousled light brown hair wearing eyeglasses.\" width=\"650\" height=\"812\" class=\"size-full wp-image-549763\" srcset=\"https:\/\/earthsky.org\/upl\/2026\/06\/Gabriel-Gowman-University-of-Arizona.jpg 650w, https:\/\/earthsky.org\/upl\/2026\/06\/Gabriel-Gowman-University-of-Arizona-240x300.jpg 240w\" sizes=\"auto, (max-width: 650px) 100vw, 650px\"\/><figcaption id=\"caption-attachment-549763\" class=\"wp-caption-text\">Gabriel Gowman at the University of Arizona is the lead author of the gravity mapping paper. Image via the University of Arizona.<\/figcaption><\/figure>\n<h3>Lots of mantle ejecta for astronauts to explore<\/h3>\n<p>Scientists had thought that the deepest part of the ejecta might be far away from the proposed landing sites in the area. But the new studies show this might not be the case. Some of the deposits could extend closer to the south polar region, including the landing sites. That\u2019s good news for the astronauts being able to sample some of those deposits.<\/p>\n<p>In 2019, scientists said they found evidence for an unusually dense mass beneath the South Pole-Aitken basin. The metallic rock is five times larger than the Big Island of Hawaii.<\/p>\n<p>On June 25, 2024, the Chinese Chang\u2019e 6 lunar probe landed in the Apollo basin, a region within the South Pole-Aitken basin. It returned samples to Earth 53 days later.<\/p>\n<p>Bottom line: Two new studies examine the South Pole-Aitken basin on the moon. This region is a future landing site for Artemis astronauts.<\/p>\n<p>Source: A southward differentiated impactor forms the tapered shape of the South Pole\u2013Aitken impact basin on the Moon<\/p>\n<p>Source: Gravity Mapping of Lunar Mantle Material in South Pole-Aitken Basin Ejecta<\/p>\n<p>Via SwRI<\/p>\n<p>Read more: Moon\u2019s largest crater is rounder than 1st thought<\/p>\n<p>Read more: What is the mystery mass on the moon?<\/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\/south-pole-aitken-basin-target-artemis-moon-missions\/?rand=772280\">Source link <\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>View larger. | This globe map shows the South Pole-Aitken basin (blue) and surrounding regions. Here we see rocks from the moon\u2019s mantle, the thick, rocky layer directly beneath its&hellip; <\/p>\n","protected":false},"author":1,"featured_media":802741,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[46],"tags":[],"class_list":["post-802740","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\/802740","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=802740"}],"version-history":[{"count":0,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/802740\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/media\/802741"}],"wp:attachment":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=802740"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=802740"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=802740"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}