{"id":211202,"date":"1988-05-22T22:05:00","date_gmt":"1988-05-22T19:05:00","guid":{"rendered":"http:\/\/www.fyysika.ee\/?guid=774ea6d8fda90ae26059aca98bf50550"},"modified":"1988-05-22T22:05:00","modified_gmt":"1988-05-22T19:05:00","slug":"venus-geological-findings","status":"publish","type":"post","link":"https:\/\/www.fyysika.ee\/?p=211202","title":{"rendered":"Venus Geological Findings"},"content":{"rendered":"<p><a href=\"http:\/\/www.jpl.nasa.gov\/news\/&#038;rn=news.xml&#038;rst=5820\"><br \/>\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/www.jpl.nasa.gov\/images\/\" align=\"left\" alt=\"NASA Jet Propulsion Laboratory, California Institute of Technology\" width=\"100\" height=\"75\" border=\"0\" \/><\/a><\/p>\n<p>\t\tNewly processed radar pictures of the surface of Venus show what may be geologically recent volcanic activity and impact cratering, including possible volcanic mountains and broad lava flows and fields like those which make up the Hawaiian Islands, JPL scientists have reported.\n\t\t<\/p>\n<p><br clear=\"all\"\/><\/p>\n","protected":false},"excerpt":{"rendered":"<p>\t\tNewly processed radar pictures of the surface of Venus show what may be geologically recent volcanic activity and impact cratering, including possible volcanic mountains and broad lava flows and fields like those which make up the Hawaii&#8230;<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_genesis_hide_title":false,"_genesis_hide_breadcrumbs":false,"_genesis_hide_singular_image":false,"_genesis_hide_footer_widgets":false,"_genesis_custom_body_class":"","_genesis_custom_post_class":"","_genesis_layout":"","footnotes":""},"categories":[179],"tags":[],"class_list":{"0":"post-211202","1":"post","2":"type-post","3":"status-publish","4":"format-standard","6":"category-rss-kosmos","7":"entry"},"_links":{"self":[{"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=\/wp\/v2\/posts\/211202","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=211202"}],"version-history":[{"count":0,"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=\/wp\/v2\/posts\/211202\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=211202"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=211202"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=211202"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}