{"id":248400,"date":"2016-12-08T06:00:00","date_gmt":"2016-12-08T10:00:00","guid":{"rendered":"http:\/\/spaceweekly.com\/?guid=bfb14dbd6d09fd287a24eb08d1054c27"},"modified":"2016-12-08T06:00:00","modified_gmt":"2016-12-08T10:00:00","slug":"fly-over-mawrth-vallis","status":"publish","type":"post","link":"https:\/\/spaceweekly.com\/?p=248400","title":{"rendered":"Fly over Mawrth Vallis"},"content":{"rendered":"<p>\t\t\t\t\t<img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/www.esa.int\/var\/esa\/storage\/images\/esa_multimedia\/videos\/2016\/12\/fly_over_mawrth_vallis\/16553199-1-eng-GB\/Fly_over_Mawrth_Vallis_small.png\" width=\"170\" height=\"96\" align=\"left\" hspace=\"8\" \/><\/p>\n<p>\nThis movie, based on images taken by ESA\u2019s Mars Express, highlights Mawrth Vallis, a 600 km-long, 2 km-deep outflow channel at the boundary of the southern highlands and the northern lowlands of Mars.\n<\/p>\n<p>\nThe movie begins at the mouth of the channel in Chryse Planitia, and heads towards the apparent source region in the Arabia Terra highlands.\n<\/p>\n<p>\nThe 4 billion year-old plateau is characterised by many impact craters, indicative of its great age.\n<\/p>\n<p>\nZooming in, patches of light and dark deposits are revealed. The light-toned layered sediments are among the largest outcrops of clay minerals \u2013 phyllosilicates \u2013 on Mars. Their presence indicates the presence of liquid water in the past.\n<\/p>\n<p>\nThe variety of water-bearing minerals and the possibility that they might contain a record of an ancient, habitable environment on Mars led scientists to propose Mawrth Vallis as a <a href=\"http:\/\/exploration.esa.int\/mars\/54721-mawrth-vallis\/\">candidate landing site for the ExoMars 2020 mission<\/a>.\n<\/p>\n<p>\nThe animation is based on a colour mosaic and digital terrain model derived from data collected by the high-resolution stereo camera on Mars Express and <a href=\"http:\/\/www.esa.int\/spaceinimages\/Images\/2016\/09\/Mawrth_Vallis_martian_mosaic\">released earlier this year<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/www.esa.int\/var\/esa\/storage\/images\/esa_multimedia\/videos\/2016\/12\/fly_over_mawrth_vallis\/16553199-1-eng-GB\/Fly_over_Mawrth_Vallis_small.png\" width=\"170\" height=\"96\" align=\"left\" hspace=\"8\"><\/p>\n<p>\nThis movie, based on images taken by ESA&rsquo;s Mars Express, highlights Mawrth Vallis, a 600 km-long, 2 km-deep outflow channel at the boundary of the southern highlands and the northern lowlands of Mars.\n<\/p>\n<p>\nThe movie begins at the mouth of the channel in Chryse Planitia, and heads towards the apparent source region in the Arabia Terra highlands.\n<\/p>\n<p>\nThe 4 billion year-old plateau is characterised by many impact craters, indicative of its great age.\n<\/p>\n<p>\nZooming in, patches of light and dark deposits are revealed. The light-toned layered sediments are among the largest outcrops of clay minerals &ndash; phyllosilicates &ndash; on Mars. Their presence indicates the presence of liquid water in the past.\n<\/p>\n<p>\nThe variety of water-bearing minerals and the possibility that they might contain a record of an ancient, habitable environment on Mars led scientists to propose Mawrth Vallis as a <a href=\"http:\/\/exploration.esa.int\/mars\/54721-mawrth-vallis\/\">candidate landing site for the ExoMars 2020 mission<\/a>.\n<\/p>\n<p>\nThe animation is based on a colour mosaic and digital terrain model derived from data collected by the high-resolution stereo camera on Mars Express and <a href=\"http:\/\/www.esa.int\/spaceinimages\/Images\/2016\/09\/Mawrth_Vallis_martian_mosaic\">released earlier this year<\/a><\/p>\n","protected":false},"author":5,"featured_media":615444,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[27],"tags":[],"class_list":["post-248400","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-multimedia"],"_links":{"self":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/248400","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\/5"}],"replies":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=248400"}],"version-history":[{"count":1,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/248400\/revisions"}],"predecessor-version":[{"id":248401,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/248400\/revisions\/248401"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/media\/615444"}],"wp:attachment":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=248400"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=248400"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=248400"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}