{"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

\natmosphere and the ocean<\/a>

\n
currents<\/a>

\n
hydrologic cycle<\/a>

\n
ocean circulation<\/a>

\n
tides<\/a>

\n
waves<\/a>

\n
world ocean<\/a>

\nChemical science

\n
\n
salinity<\/a>

\nGeological science

\n
\n
beach formation<\/a>

\n
ocean formation<\/a>

\n
plate tectonics<\/a>

\n
sea floor<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"

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}]}}