{"id":83,"date":"2012-09-28T04:18:25","date_gmt":"2012-09-28T04:18:25","guid":{"rendered":"https:\/\/staffblogs.le.ac.uk\/mars\/2012\/09\/28\/friday-28th-september-sol-52-1\/"},"modified":"2025-02-26T13:28:39","modified_gmt":"2025-02-26T13:28:39","slug":"friday-28th-september-sol-52-1","status":"publish","type":"post","link":"https:\/\/staffblogs.le.ac.uk\/mars\/2012\/09\/28\/friday-28th-september-sol-52-1\/","title":{"rendered":"Friday 28th September Sol 52"},"content":{"rendered":"<\/p>\n<p>A group us have been on a field trip between the San Andreas and San Gabriel faults, about an hour\u2019s drive north of JPL.&nbsp; Movement between these faults within the last 10 million years created a large basin filled with alluvial and marine sediments.&nbsp; This is stimulating for our current science discussions about the outcrops we have driving past and studying on our way to Glenelg.&nbsp; It makes us think of the structures and processes associated with sedimentary rocks and the measurements we need to make.&nbsp; <\/p>\n<p>Trough studying outcrops like \u2018Link\u2019 we can learn about the environment within which the water flowed to carry down and abrade the clasts.&nbsp; It can also tell us about source regions for the clasts at the margins of Gale Crater.&nbsp; Happily we have fresh surfaces which are not covered by dust, that will make our job a lot easier.&nbsp; <\/p>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>A group us have been on a field trip between the San Andreas and San Gabriel faults, about an hour\u2019s drive north of JPL.&nbsp; Movement between these faults within the last 10 million years created a large basin filled with alluvial and marine sediments.&nbsp; This is stimulating for our current science discussions about the outcrops [&hellip;]<\/p>\n","protected":false},"author":273,"featured_media":332,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-83","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\/83","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=83"}],"version-history":[{"count":1,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/posts\/83\/revisions"}],"predecessor-version":[{"id":739,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/posts\/83\/revisions\/739"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/media\/332"}],"wp:attachment":[{"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/media?parent=83"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/categories?post=83"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/staffblogs.le.ac.uk\/mars\/wp-json\/wp\/v2\/tags?post=83"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}