{"id":188,"date":"2015-11-20T15:00:53","date_gmt":"2015-11-20T20:00:53","guid":{"rendered":"http:\/\/blogs.uml.edu\/antarctica-2015\/?p=188"},"modified":"2015-11-23T23:17:41","modified_gmt":"2015-11-24T04:17:41","slug":"highlights-from-our-camp-move","status":"publish","type":"post","link":"https:\/\/blogs.uml.edu\/antarctica-2015\/2015\/11\/20\/highlights-from-our-camp-move\/","title":{"rendered":"Highlights from our camp move"},"content":{"rendered":"<div id=\"attachment_189\" style=\"width: 594px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove00.jpg\"><img aria-describedby=\"caption-attachment-189\" loading=\"lazy\" class=\"size-large wp-image-189\" src=\"http:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove00-1024x576.jpg\" alt=\"Kate flying towards Wright Valley.\" width=\"584\" height=\"329\" srcset=\"https:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove00-1024x576.jpg 1024w, https:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove00-300x169.jpg 300w, https:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove00-500x281.jpg 500w\" sizes=\"(max-width: 584px) 100vw, 584px\" \/><\/a><p id=\"caption-attachment-189\" class=\"wp-caption-text\">Kate flying towards Wright Valley.<\/p><\/div>\n<p>We\u2019ve moved to our final field location, the steep-walled, purple-hued South Fork of Wright Valley. Coming from McMurdo, you fly across the Asgard Range into Wright Valley. The bedrock of the Asgards is striking, all pale oranges with dikes and thick sills. Long lobes of flowing patterned ground stretch along many of the valleys, adding a peculiarly geometric regularity to the place.<\/p>\n<div id=\"attachment_191\" style=\"width: 594px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove01.jpg\"><img aria-describedby=\"caption-attachment-191\" loading=\"lazy\" class=\"size-large wp-image-191\" src=\"http:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove01-1024x576.jpg\" alt=\"Asgards from the helo.\" width=\"584\" height=\"329\" srcset=\"https:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove01-1024x576.jpg 1024w, https:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove01-300x169.jpg 300w, https:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove01-500x281.jpg 500w\" sizes=\"(max-width: 584px) 100vw, 584px\" \/><\/a><p id=\"caption-attachment-191\" class=\"wp-caption-text\">Asgards from the helo.<\/p><\/div>\n<div id=\"attachment_192\" style=\"width: 594px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove02.jpg\"><img aria-describedby=\"caption-attachment-192\" loading=\"lazy\" class=\"size-large wp-image-192\" src=\"http:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove02-1024x576.jpg\" alt=\"Patterned ground in the Asgards.\" width=\"584\" height=\"329\" srcset=\"https:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove02-1024x576.jpg 1024w, https:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove02-300x169.jpg 300w, https:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove02-500x281.jpg 500w\" sizes=\"(max-width: 584px) 100vw, 584px\" \/><\/a><p id=\"caption-attachment-192\" class=\"wp-caption-text\">Patterned ground in the Asgards.<\/p><\/div>\n<div id=\"attachment_193\" style=\"width: 594px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove03.jpg\"><img aria-describedby=\"caption-attachment-193\" loading=\"lazy\" class=\"size-large wp-image-193\" src=\"http:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove03-1024x576.jpg\" alt=\"Lovely orange bedrock with dikes.\" width=\"584\" height=\"329\" srcset=\"https:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove03-1024x576.jpg 1024w, https:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove03-300x169.jpg 300w, https:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove03-500x281.jpg 500w\" sizes=\"(max-width: 584px) 100vw, 584px\" \/><\/a><p id=\"caption-attachment-193\" class=\"wp-caption-text\">Lovely orange bedrock with dikes.<\/p><\/div>\n<p>Just downhill of our tents is Don Juan Pond, the saltiest natural body of water in the world. Thus, I have had the pleasure of viewing Blood Falls and Don Juan Pond straight from the door of my Scott tent.<\/p>\n<p>South Fork, and Don Juan Pond in particular, is one of Jay\u2019s favorite places in the world. The rest of us are getting pretty fond of it too, as IT\u2019S ABOVE FREEZING OMG. Miracle of miracles, the Antarctic summer has arrived.<\/p>\n<div id=\"attachment_194\" style=\"width: 594px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove04.jpg\"><img aria-describedby=\"caption-attachment-194\" loading=\"lazy\" class=\"size-large wp-image-194\" src=\"http:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove04-1024x576.jpg\" alt=\"Jay meditating on Don Juan Pond.\" width=\"584\" height=\"329\" srcset=\"https:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove04-1024x576.jpg 1024w, https:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove04-300x169.jpg 300w, https:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove04-500x281.jpg 500w\" sizes=\"(max-width: 584px) 100vw, 584px\" \/><\/a><p id=\"caption-attachment-194\" class=\"wp-caption-text\">Jay meditating on Don Juan Pond.<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>We\u2019ve moved to our final field location, the steep-walled, purple-hued South Fork of Wright Valley. Coming from McMurdo, you fly across the Asgard Range into Wright Valley. The bedrock of the Asgards is striking, all pale oranges with dikes and &hellip; <a href=\"https:\/\/blogs.uml.edu\/antarctica-2015\/2015\/11\/20\/highlights-from-our-camp-move\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":278,"featured_media":0,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":[],"categories":[1],"tags":[],"_links":{"self":[{"href":"https:\/\/blogs.uml.edu\/antarctica-2015\/wp-json\/wp\/v2\/posts\/188"}],"collection":[{"href":"https:\/\/blogs.uml.edu\/antarctica-2015\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blogs.uml.edu\/antarctica-2015\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.uml.edu\/antarctica-2015\/wp-json\/wp\/v2\/users\/278"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.uml.edu\/antarctica-2015\/wp-json\/wp\/v2\/comments?post=188"}],"version-history":[{"count":2,"href":"https:\/\/blogs.uml.edu\/antarctica-2015\/wp-json\/wp\/v2\/posts\/188\/revisions"}],"predecessor-version":[{"id":195,"href":"https:\/\/blogs.uml.edu\/antarctica-2015\/wp-json\/wp\/v2\/posts\/188\/revisions\/195"}],"wp:attachment":[{"href":"https:\/\/blogs.uml.edu\/antarctica-2015\/wp-json\/wp\/v2\/media?parent=188"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.uml.edu\/antarctica-2015\/wp-json\/wp\/v2\/categories?post=188"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.uml.edu\/antarctica-2015\/wp-json\/wp\/v2\/tags?post=188"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}