{"id":49,"date":"2016-11-14T05:34:00","date_gmt":"2016-11-14T05:34:00","guid":{"rendered":"http:\/\/blog.espol.edu.ec\/jolureye\/?p=49"},"modified":"2016-11-15T19:35:56","modified_gmt":"2016-11-15T19:35:56","slug":"volcan-tungurahua","status":"publish","type":"post","link":"https:\/\/blog.espol.edu.ec\/jolureye\/2016\/11\/14\/volcan-tungurahua\/","title":{"rendered":"Volc\u00e1n Tungurahua"},"content":{"rendered":"<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-50\" src=\"http:\/\/blog.espol.edu.ec\/jolureye\/files\/2016\/11\/Tungurahua-1-850x478.jpg\" alt=\"tungurahua-1\" width=\"850\" height=\"478\" srcset=\"https:\/\/blog.espol.edu.ec\/jolureye\/files\/2016\/11\/Tungurahua-1-850x478.jpg 850w, https:\/\/blog.espol.edu.ec\/jolureye\/files\/2016\/11\/Tungurahua-1-250x141.jpg 250w\" sizes=\"auto, (max-width: 850px) 100vw, 850px\" \/><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-52\" src=\"http:\/\/blog.espol.edu.ec\/jolureye\/files\/2016\/11\/tungurahua-850x478.jpg\" alt=\"tungurahua\" width=\"850\" height=\"478\" srcset=\"https:\/\/blog.espol.edu.ec\/jolureye\/files\/2016\/11\/tungurahua-850x478.jpg 850w, https:\/\/blog.espol.edu.ec\/jolureye\/files\/2016\/11\/tungurahua-250x141.jpg 250w, https:\/\/blog.espol.edu.ec\/jolureye\/files\/2016\/11\/tungurahua-768x432.jpg 768w, https:\/\/blog.espol.edu.ec\/jolureye\/files\/2016\/11\/tungurahua-1200x675.jpg 1200w, https:\/\/blog.espol.edu.ec\/jolureye\/files\/2016\/11\/tungurahua.jpg 1920w\" sizes=\"auto, (max-width: 850px) 100vw, 850px\" \/><\/p>\n<p>El Tungurahua es un estrato-volc\u00e1n andes\u00edtico compuesto, ubicado en la Cordillera Real del Ecuador, 120 km al sur de Quito, 33 km al SE de Ambato y tan s\u00f3lo a 8 km al Norte de la ciudad de Ba\u00f1os. Es un edificio volc\u00e1nico de 5020 m de altura con un di\u00e1metro basal de 16 km. Hall et al. (1999) dividen a este volc\u00e1n en tres edificios sucesivos, Tungurahua I, II y III, siendo el tercero el edificio actual. Los dos edificios anteriores sufrieron colapsos sectoriales hace 30 y 3 ka, cuyos dep\u00f3sitos de avalancha afloran en los valles de los r\u00edos Chambo y Patate. La actividad del Tungurahua III habr\u00eda comenzado con la emisi\u00f3n del gran flujo de lava de las Juntas hace aproximadamente 2300 a\u00f1os (Hall et al., 1999). Desde el a\u00f1o 1300 AD el Tungurahua ha producido erupciones con flujos pirocl\u00e1sticos, ca\u00eddas de ceniza, flujos de lava y lahares, al menos una vez por siglo.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>El Tungurahua es un estrato-volc\u00e1n andes\u00edtico compuesto, ubicado en la Cordillera Real del Ecuador, 120 km al sur de Quito, 33 km al SE de Ambato y tan s\u00f3lo a 8 km al Norte de la ciudad de Ba\u00f1os. Es un edificio volc\u00e1nico de 5020 m de altura con un di\u00e1metro basal de 16 km. &hellip; <\/p>\n<p><a class=\"more-link btn\" href=\"https:\/\/blog.espol.edu.ec\/jolureye\/2016\/11\/14\/volcan-tungurahua\/\">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-49","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\/49","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=49"}],"version-history":[{"count":2,"href":"https:\/\/blog.espol.edu.ec\/jolureye\/wp-json\/wp\/v2\/posts\/49\/revisions"}],"predecessor-version":[{"id":54,"href":"https:\/\/blog.espol.edu.ec\/jolureye\/wp-json\/wp\/v2\/posts\/49\/revisions\/54"}],"wp:attachment":[{"href":"https:\/\/blog.espol.edu.ec\/jolureye\/wp-json\/wp\/v2\/media?parent=49"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blog.espol.edu.ec\/jolureye\/wp-json\/wp\/v2\/categories?post=49"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blog.espol.edu.ec\/jolureye\/wp-json\/wp\/v2\/tags?post=49"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}