<\/a><\/p>\nLayers of tephra deposited during the eruption and formation of Surtsey island. The deposited layers are offset by fractures that have since filled with other material.<\/p>\n","protected":false},"excerpt":{"rendered":"
Layers of tephra deposited during the eruption and formation of Surtsey island. The deposited layers are offset by fractures that have since filled with other material.<\/p>\n","protected":false},"author":1,"featured_media":253,"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\/257"}],"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=257"}],"version-history":[{"count":3,"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=\/wp\/v2\/posts\/257\/revisions"}],"predecessor-version":[{"id":260,"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=\/wp\/v2\/posts\/257\/revisions\/260"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=\/wp\/v2\/media\/253"}],"wp:attachment":[{"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=257"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=257"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/surtsey50years.utah.edu\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=257"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}