Group C: Bay of Islands Ophiolite Complex<\/strong><\/p>\n GeoSite Group C represents sections of oceanic crust, likely developed within arcs and back arc basins in the ancient Iapetus Ocean. These have been tectonically transported across the largely sedimentary rocks of GeoSite Groups A and B. The rocks of Group C provide insight into the nature and structure of the oceanic crust, and are some of the best-known and best-preserved ophiolite suites known in the geological<\/strong> record.<\/div>[\/vc_column][\/vc_row]\n<\/div>","protected":false},"excerpt":{"rendered":" [vc_row padding_top=”0px” padding_bottom=”0px”][vc_column fade_animation_offset=”45px” width=”1\/1″][\/vc_column][\/vc_row]<\/p>\n","protected":false},"author":1,"featured_media":1022,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"_links":{"self":[{"href":"https:\/\/caboxgeopark.org\/wp-json\/wp\/v2\/pages\/319"}],"collection":[{"href":"https:\/\/caboxgeopark.org\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/caboxgeopark.org\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/caboxgeopark.org\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/caboxgeopark.org\/wp-json\/wp\/v2\/comments?post=319"}],"version-history":[{"count":5,"href":"https:\/\/caboxgeopark.org\/wp-json\/wp\/v2\/pages\/319\/revisions"}],"predecessor-version":[{"id":2600,"href":"https:\/\/caboxgeopark.org\/wp-json\/wp\/v2\/pages\/319\/revisions\/2600"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/caboxgeopark.org\/wp-json\/wp\/v2\/media\/1022"}],"wp:attachment":[{"href":"https:\/\/caboxgeopark.org\/wp-json\/wp\/v2\/media?parent=319"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}