{"id":426351,"date":"2026-05-13T22:52:17","date_gmt":"2026-05-13T22:52:17","guid":{"rendered":"https:\/\/www.newsbeep.com\/nz\/426351\/"},"modified":"2026-05-13T22:52:17","modified_gmt":"2026-05-13T22:52:17","slug":"strange-dark-material-spotted-in-an-ancient-channel-on-mars-where-water-once-flowed-3-5-billion-years-ago","status":"publish","type":"post","link":"https:\/\/www.newsbeep.com\/nz\/426351\/","title":{"rendered":"Strange, dark material spotted in an ancient channel on Mars, where water once flowed 3.5 billion years ago"},"content":{"rendered":"<p><a class=\"preferred-sources-bottom\" href=\"https:\/\/www.google.com\/preferences\/source?q=skyatnightmagazine.com\" rel=\"nofollow noopener\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" width=\"676\" height=\"213\" src=\"https:\/\/www.newsbeep.com\/nz\/wp-content\/uploads\/2026\/05\/1778712735_564_Add-us-as-a-preferred-source-1.webp\" alt=\"\" class=\"wp-image-183913\" style=\"width:168px;height:auto\"\/><\/a><\/p>\n<p>The European Space Agency&#8217;s Mars Express mission has captured an image showing a section of an ancient channel where water once flowed on Mars.<\/p>\n<p>The channel is Shalbatana Vallis, which can be found near Mars\u2019s equator, and the image shows the northern section of the channel, which is about 800 miles (1,300km) long.<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" width=\"1200\" height=\"800\" src=\"https:\/\/www.newsbeep.com\/nz\/wp-content\/uploads\/2026\/05\/1778712735_475_face-mars-nasa.jpg\" alt=\"The 'face on Mars' is a feature on Mars photographed by NASA's Viking 1 Orbiter on 25 July 1976. Credit: NASA\/JPL\" class=\"wp-image-174294\"\/>The &#8216;face on Mars&#8217; photographed by NASA&#8217;s Viking 1 Orbiter, 25 July 1976. Credit: NASA\/JPL<\/p>\n<p>Water on Mars<br \/>\n<img loading=\"lazy\" decoding=\"async\" width=\"1200\" height=\"515\" src=\"https:\/\/www.newsbeep.com\/nz\/wp-content\/uploads\/2026\/05\/Shalbatana-Vallis.jpg\" alt=\"A Mars Express image showing part of Shalbatana Vallis, a large channel in Mars\u2019s equatorial region. Credit: ESA\/DLR\/FU Berlin\" class=\"wp-image-187825\"\/>A Mars Express image showing part of Shalbatana Vallis, a large channel in Mars\u2019s equatorial region. Credit: ESA\/DLR\/FU Berlin<\/p>\n<p>While <a href=\"https:\/\/www.skyatnightmagazine.com\/astrophotography\/planets\/mars\" target=\"_blank\" rel=\"noopener nofollow\">Mars<\/a> today is a cold, barren planet with no immediate signs of life, it was once much warmer and wetter.<\/p>\n<p>Planetary scientists have discovered a wealth of evidence over the past few decades that liquid <a href=\"https:\/\/www.skyatnightmagazine.com\/space-science\/water-on-mars\" target=\"_blank\" rel=\"noopener nofollow\">water once flowed on Mars<\/a> in the form of rivers, lakes and even oceans.<\/p>\n<p>The evidence of this can be seen today, such as in the form of ancient channels like Shalbatana Vallis.<\/p>\n<p>Scientists say Shalbatana Vallis formed 3.5 billion years ago by groundwater rising up to the Martian surface in enormous quantities.<\/p>\n<p>After flooding this section of the surface of Mars, the water then ran downhill, eroding the rock and producing the winding valley seen in these images.<\/p>\n<p>The main valley is about 6 miles (10km) wide and 0.3 miles (0.5km) deep.<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" width=\"1200\" height=\"516\" src=\"https:\/\/www.newsbeep.com\/nz\/wp-content\/uploads\/2026\/05\/Shalbatana-Vallis-topographic.jpg\" alt=\"A colour-coded topographic image showing part of Shalbatana Vallis, a large channel near Mars\u2019s equator. Lower parts are shown in blues and greens, while higher regions are shown in whites and reds. Credit: ESA\/DLR\/FU Berlin\" class=\"wp-image-187824\"\/>A colour-coded topographic image showing part of Shalbatana Vallis, a large channel near Mars\u2019s equator.  Lower parts are shown in blues and greens, while higher regions are shown in whites and reds. Credit: ESA\/DLR\/FU Berlin<\/p>\n<p>Scientists say Shalbatana Vallis was likely deeper in the past, but has been filled in over centuries with different natural materials on the surface of Mars.<\/p>\n<p>This includes volcanic ash, which can be seen in Mars Express images as dark blue material, and was blown across the planet by its strong winds.<\/p>\n<p>Data from the Mars Express spacecraft was also used to capture this image, showing a strange bulge in the channel.<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" width=\"1200\" height=\"800\" src=\"https:\/\/www.newsbeep.com\/nz\/wp-content\/uploads\/2026\/05\/Shalbatana-Vallis-mars.jpg\" alt=\"A view of Shalbatana Vallis, a large channel near Mars\u2019s equator, captured by the Mars Express spacecraft. The dark material on the left of the depression is ancient volcanic ash. Credit: ESA\/DLR\/FU Berlin\" class=\"wp-image-187823\"\/>A view of Shalbatana Vallis, a large channel near Mars\u2019s equator, captured by the Mars Express spacecraft. The dark material on the left of the depression is ancient volcanic ash. Credit: ESA\/DLR\/FU Berlin<\/p>\n<p>Scientists say it probably formed when ice trapped below the surface of Mars began to melt, causing the ground to collapse.<\/p>\n<p>In the image, the dark material on the left of the bulge is volcanic ash.<\/p>\n<p>Today, Mars doesn&#8217;t have any known active volcanoes, but it is home to Olympus Mons, the largest volcano in the Solar System.<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" width=\"1200\" height=\"800\" src=\"https:\/\/www.newsbeep.com\/nz\/wp-content\/uploads\/2026\/05\/Shalbatana-Vallis-birds-eye.jpg\" alt=\"A bird's eye view of Shalbatana Vallis, a large channel near Mars\u2019s equator, captured by the Mars Express spacecraft. Credit: ESA\/DLR\/FU Berlin\" class=\"wp-image-187822\"\/>A bird&#8217;s eye view of Shalbatana Vallis, a large channel near Mars\u2019s equator, captured by the Mars Express spacecraft. Credit: ESA\/DLR\/FU Berlin<\/p>\n<p>Also visible in the image are impact craters, caused by space rocks smashing into the Martian surface.<\/p>\n<p>The rest of the terrain is smooth, which, scientists say, indicates it was once flooded by lava. In some places, this lava crumpled as it cooled, which causes the &#8216;wrinkle ridges&#8217; seen in the image.<\/p>\n","protected":false},"excerpt":{"rendered":"The European Space Agency&#8217;s Mars Express mission has captured an image showing a section of an ancient channel&hellip;\n","protected":false},"author":2,"featured_media":426352,"comment_status":"","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[23],"tags":[111,139,69,147,392],"class_list":["post-426351","post","type-post","status-publish","format-standard","has-post-thumbnail","category-space","tag-new-zealand","tag-newzealand","tag-nz","tag-science","tag-space"],"_links":{"self":[{"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/posts\/426351","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=426351"}],"version-history":[{"count":0,"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/posts\/426351\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/media\/426352"}],"wp:attachment":[{"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/media?parent=426351"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/categories?post=426351"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.newsbeep.com\/nz\/wp-json\/wp\/v2\/tags?post=426351"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}