{"id":275,"date":"2016-04-17T18:41:50","date_gmt":"2016-04-17T18:41:50","guid":{"rendered":"https:\/\/staffblogs.le.ac.uk\/mars\/2016\/04\/17\/17th-april-2016-sol-1315\/"},"modified":"2025-02-26T13:28:36","modified_gmt":"2025-02-26T13:28:36","slug":"17th-april-2016-sol-1315","status":"publish","type":"post","link":"https:\/\/staffblogs.le.ac.uk\/mars\/2016\/04\/17\/17th-april-2016-sol-1315\/","title":{"rendered":"17th April 2016 Sol 1315"},"content":{"rendered":"<p>Here is a NavCam mosaic of the Naukluft Plateau. \u00a0We are looking around us for the next drill target. A particular feature is searching for, and trying to understand, silica enrichments. \u00a0The formation we are driving over is called the Stimson and is thought to have formed from ancient wind blown sediments which cut down through the underlying \u00a0lake deposits of the Murray formation. Are these silica enrichments due to late alteration along fractures or was some of it blown in with the other Stimson grains?<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Here is a NavCam mosaic of the Naukluft Plateau. \u00a0We are looking around us for the next drill target. A particular feature is searching for, and trying to understand, silica enrichments. \u00a0The formation we are driving over is called the Stimson and is thought to have formed from ancient wind blown sediments which cut down [&hellip;]<\/p>\n","protected":false},"author":273,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-275","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"_links":{"self":[{"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/posts\/275","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=275"}],"version-history":[{"count":1,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/posts\/275\/revisions"}],"predecessor-version":[{"id":547,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/posts\/275\/revisions\/547"}],"wp:attachment":[{"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/media?parent=275"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/categories?post=275"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/tags?post=275"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}