{"id":621108,"date":"2026-10-05T09:06:10","date_gmt":"2026-10-05T09:06:10","guid":{"rendered":"https:\/\/www.newsbeep.com\/nz\/621108\/"},"modified":"2026-10-05T09:06:10","modified_gmt":"2026-10-05T09:06:10","slug":"moon-like-madagascar-nasa-science","status":"publish","type":"post","link":"https:\/\/www.newsbeep.com\/nz\/621108\/","title":{"rendered":"Moon-Like Madagascar &#8211; NASA Science"},"content":{"rendered":"<p class=\"wp-block-paragraph\">From an astronaut\u2019s perspective looking back at Earth, a patch of bright rock in arid southern Madagascar may appear out of place. But it wouldn\u2019t on the Moon. The igneous rock anorthosite, common on the Moon\u2019s surface, is visible from Earth with the unaided eye as the light-colored, highly reflective areas known as the <a href=\"https:\/\/earthandsolarsystem.wordpress.com\/2017\/07\/27\/new-group-paper-impact-shock-state-of-the-lunar-highlands\/\" rel=\"nofollow noopener\" target=\"_blank\">lunar highlands<\/a>. Anorthosite also crops up across Earth\u2019s surface, from eastern Canada and Scandinavia to southern India and Madagascar, where it forms a striking round feature.<\/p>\n<p class=\"wp-block-paragraph\">An astronaut aboard the International Space Station captured this photo of the Saririaky anorthosite <a href=\"https:\/\/www.worldatlas.com\/articles\/what-is-a-massif.html\" rel=\"nofollow noopener\" target=\"_blank\">massif<\/a> on August 28, 2026. Anorthosite is an intrusive igneous rock\u2014formed from magma that cools beneath the surface\u2014made up of large mineral crystals. <a href=\"https:\/\/doi.org\/10.1007\/s004100050461\" rel=\"nofollow noopener\" target=\"_blank\">Scientists think<\/a> the massif seen here formed in the late Precambrian, at least 600 million years ago. Its present-day outcrop covers about 100 square kilometers (40 square miles).<\/p>\n<p class=\"wp-block-paragraph\">The rocks surrounding the anorthosite reveal a dynamic chapter in the area\u2019s geologic past. Researchers have <a href=\"https:\/\/www.academia.edu\/figures\/35507545\/figure-8-detailed-foliation-trajectories-from-sector\" rel=\"nofollow noopener\" target=\"_blank\">determined<\/a> that the Saririaky massif lies within a <a href=\"https:\/\/www.sciencedirect.com\/science\/chapter\/edited-volume\/abs\/pii\/B9780128168028000020\" rel=\"nofollow noopener\" target=\"_blank\">ductile shear zone<\/a>, where high pressures and temperatures <a href=\"https:\/\/education.nationalgeographic.org\/resource\/metamorphic-rocks\/\" rel=\"nofollow noopener\" target=\"_blank\">metamorphosed<\/a> and reshaped the rock, imparting north-south-trending linear patterns.<\/p>\n<p class=\"wp-block-paragraph\">Geologists think this deformation occurred when pieces of what are now Africa, India, Madagascar, Australia, and Antarctica were colliding to form the supercontinent <a href=\"https:\/\/www.livescience.com\/37285-gondwana.html\" rel=\"nofollow noopener\" target=\"_blank\">Gondwana<\/a>. Some scientists have posited that <a href=\"https:\/\/www.researchgate.net\/figure\/a-Landsat-Thematic-Mapper-image-Scenes-160-76-and-160-77-showing-the-Ampanihy-ductile_fig1_345355691\" rel=\"nofollow noopener\" target=\"_blank\">another anorthosite massif<\/a> in the shear zone, located about 60 kilometers (40 miles) to the north, was pulled apart from the Saririaky massif in the process, creating a large-scale <a href=\"https:\/\/blogs.egu.eu\/divisions\/ts\/2019\/05\/19\/features-from-the-field-boudinage\/\" rel=\"nofollow noopener\" target=\"_blank\">boudinage<\/a> structure.<\/p>\n<p class=\"wp-block-paragraph\">Anorthosites on Earth have proven useful for scientists studying the Moon\u2019s past. <a href=\"https:\/\/www.lpi.usra.edu\/exploration\/publications\/Lunar_Highlands_Handout.pdf\" rel=\"nofollow noopener\" target=\"_blank\">Lunar anorthosites<\/a> are more than 4 billion years old, having crystallized from the Moon\u2019s <a href=\"https:\/\/en.wikipedia.org\/wiki\/Lunar_magma_ocean\" rel=\"nofollow noopener\" target=\"_blank\">magma ocean<\/a> to form its outer crust. Researchers have analyzed samples brought back to Earth by Apollo astronauts, but because that material is limited, they also look to analogous terrestrial rocks. The anorthosites in the Beartooth Mountains of Montana <a href=\"https:\/\/science.nasa.gov\/earth\/earth-observatory\/montanas-moon-like-rocks-146650\/\" rel=\"nofollow noopener\" target=\"_blank\">match the composition<\/a> of the lunar version particularly well.\u00a0<\/p>\n<p class=\"wp-block-paragraph\">Astronaut photograph <a href=\"https:\/\/eol.jsc.nasa.gov\/SearchPhotos\/photo.pl?mission=ISS075&amp;roll=E&amp;frame=85249\" rel=\"nofollow noopener\" target=\"_blank\">ISS075-E-85249<\/a> was acquired on August 28, 2026, with a Nikon Z9 digital camera using a focal length of 400 millimeters. It is provided by the ISS Crew Earth Observations Facility and the Earth Science and Remote Sensing Unit at NASA Johnson Space Center. The image was taken by a member of the\u00a0<a href=\"https:\/\/www.nasa.gov\/mission\/expedition-75\/\" rel=\"nofollow noopener\" target=\"_blank\">Expedition 75 crew<\/a>. The image has been cropped and enhanced to improve contrast, and lens artifacts have been removed. The\u00a0<a href=\"https:\/\/www.nasa.gov\/international-space-station\/\" rel=\"nofollow noopener\" target=\"_blank\">International Space Station Program<\/a>\u00a0supports the laboratory as part of the\u00a0<a href=\"https:\/\/www.nasa.gov\/international-space-station\/space-station-research-and-technology\/iss-national-laboratory\/\" rel=\"nofollow noopener\" target=\"_blank\">ISS National Lab<\/a>\u00a0to help astronauts take pictures of Earth that will be of the greatest value to scientists and the public, and to make those images freely available on the internet. Additional images taken by astronauts and cosmonauts can be viewed at the NASA\/JSC\u00a0<a href=\"https:\/\/eol.jsc.nasa.gov\/\" rel=\"nofollow noopener\" target=\"_blank\">Gateway to Astronaut Photography of Earth<\/a>. Story by Lindsey Doermann.<\/p>\n<p>\t\t\t\t\t<img width=\"8256\" height=\"5504\" src=\"https:\/\/www.newsbeep.com\/nz\/wp-content\/uploads\/2026\/10\/ISS075-E-85249_lrg.jpg\" class=\"attachment-thumbnail size-thumbnail\" alt=\"A round, white rock outcrop is surrounded by orange rocks with a north-south linear pattern. Branching riverbeds cut through the rock structures.\" style=\"transform: scale(1.2); transform-origin: 50% 50%; object-position: 50% 50%; object-fit: cover;\" block_context=\"nasa-block\" loading=\"lazy\" data-video-loop=\"\" decoding=\"async\"  \/>\t\t\t\t<\/p>\n<p>Ashwal, L.D., et al. (1998) <a href=\"https:\/\/doi.org\/10.1007\/s004100050461\" rel=\"nofollow noopener\" target=\"_blank\">Geology, petrology and isotope geochemistry of massif-type anorthosites from southwest Madagascar<\/a>. Contributions to Mineralogy and Petrology, 133, 389-401.<\/p>\n<p>Earth &amp; Solar System (2017, July 27) <a href=\"https:\/\/earthandsolarsystem.wordpress.com\/2017\/07\/27\/new-group-paper-impact-shock-state-of-the-lunar-highlands\/\" rel=\"nofollow noopener\" target=\"_blank\">Impact Shock State of the Lunar Highlands<\/a>. Accessed October 2, 2026.<\/p>\n<p>Martelat, J., et al. (2000) <a href=\"https:\/\/doi.org\/10.1016\/S0301-9268(99)00083-2\" rel=\"nofollow noopener\" target=\"_blank\">Strain pattern and late Precambrian deformation history in southern Madagascar<\/a>. Precambrian Research, 102, 1\u20132.<\/p>\n<p>NASA Earth Observatory (2020, May 4) <a href=\"https:\/\/science.nasa.gov\/earth\/earth-observatory\/montanas-moon-like-rocks-146650\/\" rel=\"nofollow noopener\" target=\"_blank\">Montana\u2019s Moon-Like Rocks<\/a>. Accessed October 2, 2026.<\/p>\n","protected":false},"excerpt":{"rendered":"From an astronaut\u2019s perspective looking back at Earth, a patch of bright rock in arid southern Madagascar may&hellip;\n","protected":false},"author":2,"featured_media":621109,"comment_status":"","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[23],"tags":[104562,168783,6692,111,139,69,147,392],"class_list":["post-621108","post","type-post","status-publish","format-standard","has-post-thumbnail","category-space","tag-earth-observatory","tag-earth-surface-interior","tag-international-space-station-iss","tag-new-zealand","tag-newzealand","tag-nz","tag-science","tag-space"],"_links":{"self":[{"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/posts\/621108","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/comments?post=621108"}],"version-history":[{"count":0,"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/posts\/621108\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/media\/621109"}],"wp:attachment":[{"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/media?parent=621108"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/categories?post=621108"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/tags?post=621108"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}