<\/a><\/p>\nView is of the inside of the eastern crater on Surtsey island. The walls of this crater are made of many layers of basaltic rock.<\/p>\n","protected":false},"excerpt":{"rendered":"
View is of the inside of the eastern crater on Surtsey island. The walls of this crater are made of many layers of basaltic rock.<\/p>\n","protected":false},"author":1,"featured_media":377,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":[],"categories":[11,13],"tags":[],"_links":{"self":[{"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=\/wp\/v2\/posts\/382"}],"collection":[{"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=382"}],"version-history":[{"count":1,"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=\/wp\/v2\/posts\/382\/revisions"}],"predecessor-version":[{"id":383,"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=\/wp\/v2\/posts\/382\/revisions\/383"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=\/wp\/v2\/media\/377"}],"wp:attachment":[{"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=382"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=382"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=382"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}