{"670991":{"#nid":"670991","#data":{"uid":"34528","author":"jhunt7","created_gmt":"2023-06-16 20:13:57","changed_gmt":"2023-06-16 20:13:57","title":"Regional topographic relief map. (Naif et al)","body":[{"value":"\u003Cp\u003E\u003Cspan\u003E\u003Cspan\u003E\u003Cspan\u003E\u003Cstrong\u003E\u003Cspan\u003E\u003Cspan\u003EFrom the study: \u003C\/span\u003E\u003C\/span\u003E\u003C\/strong\u003E\u003C\/span\u003E\u003C\/span\u003E\u003C\/span\u003E\u003Cspan\u003E\u003Cspan\u003E\u003Cspan\u003E\u003Cspan\u003E\u003Cspan\u003E\u003Cspan\u003EThe Cocos and Nazca plates are formed at the EPR and the GSC. The Gal\u00e1pagos Triple Junction (GTJ) trace marks the boundary between EPR- and GSC-derived oceanic crusts. The Gal\u00e1pagos Plume is currently centered beneath the Gal\u00e1pagos Islands 200 km south of the GSC and generates two hot spot tracks, the Cocos Ridge and the Carnegie Ridge. \u003C\/span\u003E\u003C\/span\u003E\u003C\/span\u003E\u003C\/span\u003E\u003C\/span\u003E\u003C\/span\u003E\u003C\/p\u003E\r\n","format":"limited_html"}],"image":{"alt":"Regional topographic relief map. ","view":{"#theme":"field","#title":"Image","#label_display":"hidden","#view_mode":"image_740","#language":"en","#field_name":"field_image","#field_type":"image","#field_translatable":false,"#entity_type":"media","#bundle":"image","#object":{},"#items":{},"#formatter":"image","#is_multiple":false,"#third_party_settings":[],"0":{"#theme":"image_formatter","#item":{},"#item_attributes":[],"#image_style":"large","#url":null,"#cache":{"tags":["config:image.style.large","file:253978"],"contexts":[],"max-age":-1}},"#cache":{"contexts":[],"tags":[],"max-age":-1},"#weight":0},"file":{"fid":"253978","name":"sciadv.add3761-f1.jpg","path":"\/sites\/default\/files\/2023\/06\/16\/sciadv.add3761-f1.jpg","fullpath":"\/var\/www\/html\/files\/public\/2023\/06\/16\/sciadv.add3761-f1.jpg","mime":"image\/jpeg","size":3610537}},"groups":[{"id":"1278","name":"College of Sciences"}],"keywords":[]}}}