{"id":2,"date":"2010-06-18T11:12:40","date_gmt":"2010-06-18T11:12:40","guid":{"rendered":""},"modified":"2010-11-24T10:51:21","modified_gmt":"2010-11-24T10:51:21","slug":"about-me","status":"publish","type":"page","link":"https:\/\/uni.hi.is\/rikke\/about-me\/","title":{"rendered":"About me"},"content":{"rendered":"<p><strong><a href=\"http:\/\/uni.hi.is\/rikke\/files\/2010\/06\/Rikke.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-70\" title=\"Rikke\" src=\"http:\/\/uni.hi.is\/rikke\/files\/2010\/06\/Rikke-300x199.jpg\" alt=\"\" width=\"300\" height=\"199\" srcset=\"https:\/\/uni.hi.is\/rikke\/files\/2010\/06\/Rikke-300x199.jpg 300w, https:\/\/uni.hi.is\/rikke\/files\/2010\/06\/Rikke-1024x681.jpg 1024w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><\/strong><\/p>\n<p><strong>Rikke Pedersen<\/strong><\/p>\n<p>Daily manager of <a title=\"Nordvulk\" href=\"http:\/\/www2.norvol.hi.is\/\" target=\"_blank\">Nordic Volcanological Center, University of Iceland<\/a><\/p>\n<p>Nationality: Danish; \u00a0Resident of Iceland since 2000<\/p>\n<p><strong>Research interests:<\/strong><\/p>\n<ul>\n<li>Deformation of active volcanic areas, including spreading plate boundaries<\/li>\n<li>Rheological structure of the crust and mantle beneath Iceland<\/li>\n<li>Geometrical effects of rheological boundaries on surface deformation<\/li>\n<li>Magma plumbing systems<\/li>\n<li>Finite element method (FEM) models of volcanic systems<\/li>\n<\/ul>\n<p><strong>Administrative responsibilities:<\/strong><\/p>\n<ul>\n<li>Daily management of the stipendiate programme at NORDVULK<\/li>\n<li>Contact person for media from the Nordic countries<\/li>\n<li>NORDVULK summerschools<\/li>\n<\/ul>\n","protected":false},"excerpt":{"rendered":"<p>Rikke Pedersen Daily manager of Nordic Volcanological Center, University of Iceland Nationality: Danish; \u00a0Resident of Iceland since 2000 Research interests: Deformation of active volcanic areas, including spreading plate boundaries Rheological structure of the crust and mantle beneath Iceland Geometrical effects of rheological boundaries on surface deformation Magma plumbing systems Finite element method (FEM) models of [&hellip;]<\/p>\n","protected":false},"author":194,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"open","template":"","meta":{"footnotes":""},"class_list":["post-2","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/uni.hi.is\/rikke\/wp-json\/wp\/v2\/pages\/2","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/uni.hi.is\/rikke\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/uni.hi.is\/rikke\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/uni.hi.is\/rikke\/wp-json\/wp\/v2\/users\/194"}],"replies":[{"embeddable":true,"href":"https:\/\/uni.hi.is\/rikke\/wp-json\/wp\/v2\/comments?post=2"}],"version-history":[{"count":9,"href":"https:\/\/uni.hi.is\/rikke\/wp-json\/wp\/v2\/pages\/2\/revisions"}],"predecessor-version":[{"id":73,"href":"https:\/\/uni.hi.is\/rikke\/wp-json\/wp\/v2\/pages\/2\/revisions\/73"}],"wp:attachment":[{"href":"https:\/\/uni.hi.is\/rikke\/wp-json\/wp\/v2\/media?parent=2"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}