{"id":45,"date":"2016-11-14T05:23:24","date_gmt":"2016-11-14T05:23:24","guid":{"rendered":"http:\/\/blog.espol.edu.ec\/jolureye\/?p=45"},"modified":"2016-11-15T19:36:19","modified_gmt":"2016-11-15T19:36:19","slug":"volcan-cotopaxi","status":"publish","type":"post","link":"https:\/\/blog.espol.edu.ec\/jolureye\/2016\/11\/14\/volcan-cotopaxi\/","title":{"rendered":"Volc\u00e1n Cotopaxi"},"content":{"rendered":"<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-46\" src=\"http:\/\/blog.espol.edu.ec\/jolureye\/files\/2016\/11\/Cotopaxi-800x478.jpg\" alt=\"cotopaxi\" width=\"800\" height=\"478\" \/><\/p>\n<p>El Cotopaxi se encuentra sobre la Cordillera Oriental (Real), a una distancia de 35 km al Noreste de Latacunga y de 45 km al Sureste de Quito. Su edificio con una altura de 5897 msnm, forma un cono sim\u00e9trico con pendientes de hasta 35\u00b0 y un di\u00e1metro basal de ~20 km, mientras que el di\u00e1metro del cr\u00e1ter var\u00eda entre 800 m en sentido Norte-Sur y 650 m en sentido Este-Oeste. El Cotopaxi est\u00e1 rodeado por p\u00e1ramos que bordean los 3000 msnm y por otros volcanes como Sincholahua (4873 msnm), Quilinda\u00f1a (4876 msnm) y Rumi\u00f1ahui (4722 msnm).<\/p>\n","protected":false},"excerpt":{"rendered":"<p>El Cotopaxi se encuentra sobre la Cordillera Oriental (Real), a una distancia de 35 km al Noreste de Latacunga y de 45 km al Sureste de Quito. Su edificio con una altura de 5897 msnm, forma un cono sim\u00e9trico con pendientes de hasta 35\u00b0 y un di\u00e1metro basal de ~20 km, mientras que el di\u00e1metro &hellip; <\/p>\n<p><a class=\"more-link btn\" href=\"https:\/\/blog.espol.edu.ec\/jolureye\/2016\/11\/14\/volcan-cotopaxi\/\">Seguir leyendo<\/a><\/p>\n","protected":false},"author":10723,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1399838],"tags":[],"class_list":["post-45","post","type-post","status-publish","format-standard","hentry","category-vulcanologia","item-wrap"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/blog.espol.edu.ec\/jolureye\/wp-json\/wp\/v2\/posts\/45","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blog.espol.edu.ec\/jolureye\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blog.espol.edu.ec\/jolureye\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blog.espol.edu.ec\/jolureye\/wp-json\/wp\/v2\/users\/10723"}],"replies":[{"embeddable":true,"href":"https:\/\/blog.espol.edu.ec\/jolureye\/wp-json\/wp\/v2\/comments?post=45"}],"version-history":[{"count":2,"href":"https:\/\/blog.espol.edu.ec\/jolureye\/wp-json\/wp\/v2\/posts\/45\/revisions"}],"predecessor-version":[{"id":48,"href":"https:\/\/blog.espol.edu.ec\/jolureye\/wp-json\/wp\/v2\/posts\/45\/revisions\/48"}],"wp:attachment":[{"href":"https:\/\/blog.espol.edu.ec\/jolureye\/wp-json\/wp\/v2\/media?parent=45"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blog.espol.edu.ec\/jolureye\/wp-json\/wp\/v2\/categories?post=45"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blog.espol.edu.ec\/jolureye\/wp-json\/wp\/v2\/tags?post=45"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}