{"id":169,"date":"2013-11-01T21:21:16","date_gmt":"2013-11-01T21:21:16","guid":{"rendered":"https:\/\/staffblogs.le.ac.uk\/mars\/2013\/11\/01\/1st-november-2013-sol-439\/"},"modified":"2025-02-26T13:28:38","modified_gmt":"2025-02-26T13:28:38","slug":"1st-november-2013-sol-439","status":"publish","type":"post","link":"https:\/\/staffblogs.le.ac.uk\/mars\/2013\/11\/01\/1st-november-2013-sol-439\/","title":{"rendered":"1st November 2013 Sol 439"},"content":{"rendered":"<p>We have driven right up to the Cooperstown outcrop.\u00a0 The rdige (a few tens of cm high) is composed of a resistant layer of sedimentary rock.\u00a0 This is the most extensive and detailed sedimentary outcrop since we left Yellowknife Bay.<\/p>\n<p>Its also a\u00a0 fantastic view of the crater rim,\u00a0a bit dusty but you can see what look like ancient landslides as the rim has degraded over billions of years since Gale Crater formed about 3.6 billion years ago.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>We have driven right up to the Cooperstown outcrop.\u00a0 The rdige (a few tens of cm high) is composed of a resistant layer of sedimentary rock.\u00a0 This is the most extensive and detailed sedimentary outcrop since we left Yellowknife Bay. Its also a\u00a0 fantastic view of the crater rim,\u00a0a bit dusty but you can see [&hellip;]<\/p>\n","protected":false},"author":273,"featured_media":410,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-169","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-uncategorized"],"_links":{"self":[{"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/posts\/169","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/users\/273"}],"replies":[{"embeddable":true,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/comments?post=169"}],"version-history":[{"count":1,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/posts\/169\/revisions"}],"predecessor-version":[{"id":653,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/posts\/169\/revisions\/653"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/media\/410"}],"wp:attachment":[{"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/media?parent=169"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/categories?post=169"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/tags?post=169"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}