{"id":1938,"date":"2012-11-29T23:03:06","date_gmt":"2012-11-30T04:03:06","guid":{"rendered":"http:\/\/blogs.library.mcgill.ca\/schulich\/?p=1938"},"modified":"2013-06-18T14:33:05","modified_gmt":"2013-06-18T18:33:05","slug":"nasa-news-mercury-water-ice","status":"publish","type":"post","link":"https:\/\/blogs.library.mcgill.ca\/schulich\/nasa-news-mercury-water-ice\/","title":{"rendered":"NASA news: Mercury water ice"},"content":{"rendered":"<p style=\"text-align: center;\"><a href=\"http:\/\/blogs.library.mcgill.ca\/schulich\/files\/2012\/11\/708626main_PressConf20121126_full_34x3_800-600.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-1952 aligncenter\" title=\"MercuryNorthPole\" src=\"http:\/\/blogs.library.mcgill.ca\/schulich\/files\/2012\/11\/708626main_PressConf20121126_full_34x3_800-600-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/blogs.library.mcgill.ca\/schulich\/files\/2012\/11\/708626main_PressConf20121126_full_34x3_800-600-300x225.jpg 300w, https:\/\/blogs.library.mcgill.ca\/schulich\/files\/2012\/11\/708626main_PressConf20121126_full_34x3_800-600-400x300.jpg 400w, https:\/\/blogs.library.mcgill.ca\/schulich\/files\/2012\/11\/708626main_PressConf20121126_full_34x3_800-600.jpg 960w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a>NASA held a <a href=\"http:\/\/www.nasa.gov\/home\/hqnews\/2012\/nov\/HQ_M12-219_MESSENGER_Nov-29_News_Conference.html\"> news conference<\/a> today, unveiling <a href=\"http:\/\/www.nasa.gov\/mission_pages\/messenger\/media\/PressConf20121129.html\">new evidence for water ice<\/a> at Mercury&#8217;s polar regions from the MESSENGER spacecraft.<\/p>\n<p>MESSENGER is an acronym for MErcury Surface, Space ENvironment, GEochemistry and Ranging. Powered by two solar panels, it was launched August 3, 2004, reaching Mercury&#8217;s orbit March 18, 2011 (UTC).<\/p>\n<p>Mercury has a temperature range of 610 degrees Celsius:\u00a0427 degrees on the side closest to the Sun, and -183 degrees on the night side. There are crater floors around Mercury\u2019s poles that are in persistent shade, since its rotation axis does not tilt. NASA&#8217;s latest data points to water ice and other frozen deposits in these craters.<\/p>\n<p>The red areas in this image are the permanently shadowed craters of Mercury&#8217;s north pole, with the polar deposits in yellow.<\/p>\n<div>\n<div id=\"caption_region\">\n<div>\n<p><em>Image: <a href=\"http:\/\/www.nasa.gov\/mission_pages\/messenger\/multimedia\/PressConf20121126_3.html\">NASA\/Johns Hopkins University Applied Physics Laboratory\/Carnegie Institution of Washington\/National Astronomy and Ionosphere Center, Arecibo Observatory<\/a><\/em><\/p>\n<\/div>\n<\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>NASA held a news conference today, unveiling new evidence for water ice at Mercury&#8217;s polar regions from the MESSENGER spacecraft. MESSENGER is an acronym for MErcury Surface, Space ENvironment, GEochemistry and Ranging. Powered by two solar panels, it was launched &hellip; <a href=\"https:\/\/blogs.library.mcgill.ca\/schulich\/nasa-news-mercury-water-ice\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":13,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_monsterinsights_skip_tracking":false,"_monsterinsights_sitenote_active":false,"_monsterinsights_sitenote_note":"","_monsterinsights_sitenote_category":0,"footnotes":""},"categories":[1],"tags":[155,73,65],"class_list":["post-1938","post","type-post","status-publish","format-standard","hentry","category-blog","tag-mercury","tag-nasa","tag-planets"],"_links":{"self":[{"href":"https:\/\/blogs.library.mcgill.ca\/schulich\/wp-json\/wp\/v2\/posts\/1938","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blogs.library.mcgill.ca\/schulich\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blogs.library.mcgill.ca\/schulich\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.library.mcgill.ca\/schulich\/wp-json\/wp\/v2\/users\/13"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.library.mcgill.ca\/schulich\/wp-json\/wp\/v2\/comments?post=1938"}],"version-history":[{"count":15,"href":"https:\/\/blogs.library.mcgill.ca\/schulich\/wp-json\/wp\/v2\/posts\/1938\/revisions"}],"predecessor-version":[{"id":3173,"href":"https:\/\/blogs.library.mcgill.ca\/schulich\/wp-json\/wp\/v2\/posts\/1938\/revisions\/3173"}],"wp:attachment":[{"href":"https:\/\/blogs.library.mcgill.ca\/schulich\/wp-json\/wp\/v2\/media?parent=1938"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.library.mcgill.ca\/schulich\/wp-json\/wp\/v2\/categories?post=1938"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.library.mcgill.ca\/schulich\/wp-json\/wp\/v2\/tags?post=1938"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}