{"id":3464,"date":"2019-10-02T19:17:05","date_gmt":"2019-10-02T19:17:05","guid":{"rendered":"http:\/\/www.forsea.org\/?page_id=3464"},"modified":"2019-11-06T19:33:38","modified_gmt":"2019-11-06T19:33:38","slug":"physical-science","status":"publish","type":"page","link":"http:\/\/www.forsea.org\/physical-science\/","title":{"rendered":"Physical Science"},"content":{"rendered":"
Earth science Earth science atmosphere and the ocean currents hydrologic cycle […]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"template_8.php","meta":{"footnotes":""},"_links":{"self":[{"href":"http:\/\/www.forsea.org\/wp-json\/wp\/v2\/pages\/3464"}],"collection":[{"href":"http:\/\/www.forsea.org\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"http:\/\/www.forsea.org\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"http:\/\/www.forsea.org\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"http:\/\/www.forsea.org\/wp-json\/wp\/v2\/comments?post=3464"}],"version-history":[{"count":19,"href":"http:\/\/www.forsea.org\/wp-json\/wp\/v2\/pages\/3464\/revisions"}],"predecessor-version":[{"id":5619,"href":"http:\/\/www.forsea.org\/wp-json\/wp\/v2\/pages\/3464\/revisions\/5619"}],"wp:attachment":[{"href":"http:\/\/www.forsea.org\/wp-json\/wp\/v2\/media?parent=3464"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}
\natmosphere and the ocean<\/a>
\ncurrents<\/a>
\nhydrologic cycle<\/a>
\nocean circulation<\/a>
\ntides<\/a>
\nwaves<\/a>
\nworld ocean<\/a>
\nChemical science
\n
\nsalinity<\/a>
\nGeological science
\n
\nbeach formation<\/a>
\nocean formation<\/a>
\nplate tectonics<\/a>
\nsea floor<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"