{"id":196223,"date":"2013-05-02T05:00:00","date_gmt":"2013-05-02T09:00:00","guid":{"rendered":"2a77ad2d0b3b9041708b24e095b59422"},"modified":"2013-05-02T05:00:00","modified_gmt":"2013-05-02T09:00:00","slug":"sulci-gordii","status":"publish","type":"post","link":"https:\/\/spaceweekly.com\/?p=196223","title":{"rendered":"Sulci Gordii"},"content":{"rendered":"<p>\t\t\t\t\t<img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/www.esa.int\/var\/esa\/storage\/images\/esa_multimedia\/images\/2013\/05\/sulci_gordii\/12657192-7-eng-GB\/Sulci_Gordii_small.jpg\" width=\"170\" height=\"96\" align=\"left\" hspace=\"8\" \/><\/p>\n<p>\nESA\u2019s Mars Express imaged the Sulci Gordii region of Mars with its High Resolution Stereo Camera on 23 January 2013 (orbit 11531), with a ground resolution of about 31 m per pixel. Sulci Gordii lies at approximately 17\u00b0N \/ 234\u00b0E, about 200 km east of Olympus Mons.\n<\/p>\n<p>\nThe feature is an \u2018aureole\u2019 deposit resulting from a massive landslide that sloughed away from the flanks of Olympus Mons in its distant past. The complex scene is dominated by a series of roughly parallel ridges and valleys (called sulci), with lava or water-carved channels in the southern most (left) portion of the image. Smooth, young volcanic lava flows overlay parts of the sulci.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>\t\t\t\t\t<img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/www.esa.int\/var\/esa\/storage\/images\/esa_multimedia\/images\/2013\/05\/sulci_gordii\/12657192-7-eng-GB\/Sulci_Gordii_small.jpg\" width=\"170\" height=\"96\" align=\"left\" hspace=\"8\" \/><\/p>\n<p>\nESA\u2019s Mars Express imaged the Sulci Gordii region of Mars with its High Resolution Stereo Camera on 23 January 2013 (orbit 11531), with a ground resolution of about 31 m per pixel. Sulci Gordii lies at approximately 17\u00b0N \/ 234\u00b0E, about 200 km east of Olympus Mons.\n<\/p>\n<p>\nThe feature is an \u2018aureole\u2019 deposit resulting from a massive landslide that sloughed away from the flanks of Olympus Mons in its distant past. The complex scene is dominated by a series of roughly parallel ridges and valleys (called sulci), with lava or water-carved channels in the southern most (left) portion of the image. Smooth, young volcanic lava flows overlay parts of the sulci.<\/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-196223","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\/196223","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=196223"}],"version-history":[{"count":0,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/196223\/revisions"}],"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=196223"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=196223"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=196223"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}