{"id":215,"date":"2018-08-20T18:27:04","date_gmt":"2018-08-20T18:27:04","guid":{"rendered":"http:\/\/sites.ipleiria.pt\/seismicknowledge\/?p=215"},"modified":"2018-08-29T11:19:27","modified_gmt":"2018-08-29T11:19:27","slug":"zona-del-rift-de-baikal","status":"publish","type":"post","link":"https:\/\/sites.ipleiria.pt\/seismicknowledge\/zona-del-rift-de-baikal\/","title":{"rendered":"Zona del Rift de Baikal"},"content":{"rendered":"<p>Esta falla de 1.500 kil\u00f3metros de largo tiene una parte central llena de agua: el lago Baikal. Seg\u00fan los ge\u00f3logos, esta grieta es el resultado de la divergencia de las placas Euroasi\u00e1tica y Amuria.<\/p>\n<div id=\"attachment_216\" style=\"width: 810px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-216\" class=\"size-full wp-image-216\" src=\"http:\/\/sites.ipleiria.pt\/seismicknowledge\/files\/2018\/08\/La-zona-del-Rift-de-Baikal.jpg\" alt=\"\" width=\"800\" height=\"599\" srcset=\"https:\/\/sites.ipleiria.pt\/seismicknowledge\/files\/2018\/08\/La-zona-del-Rift-de-Baikal.jpg 800w, https:\/\/sites.ipleiria.pt\/seismicknowledge\/files\/2018\/08\/La-zona-del-Rift-de-Baikal-300x225.jpg 300w, https:\/\/sites.ipleiria.pt\/seismicknowledge\/files\/2018\/08\/La-zona-del-Rift-de-Baikal-768x575.jpg 768w, https:\/\/sites.ipleiria.pt\/seismicknowledge\/files\/2018\/08\/La-zona-del-Rift-de-Baikal-370x277.jpg 370w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><p id=\"caption-attachment-216\" class=\"wp-caption-text\">La zona del Rift de Baikal<\/p><\/div>\n<p>El principal peligro en la zona, como en el caso del Kivu, se encuentra en el fondo del lago. De hecho, el fondo del lago Baikal es una falla tect\u00f3nica, y sus costas est\u00e1n constantemente alej\u00e1ndose. Los cient\u00edficos predicen que en unos cientos de millones de a\u00f1os, el Baikal se convertir\u00e1 en un oc\u00e9ano.<\/p>","protected":false},"excerpt":{"rendered":"<p>Esta falla de 1.500 kil\u00f3metros de largo tiene una parte central llena de agua: el lago Baikal. Seg\u00fan los ge\u00f3logos, esta grieta es el resultado de la divergencia de las placas Euroasi\u00e1tica y Amuria. El principal peligro en la zona,&hellip;  <\/p>\n<p class=\"more-link\"><a href=\"https:\/\/sites.ipleiria.pt\/seismicknowledge\/zona-del-rift-de-baikal\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":3142,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[112229],"tags":[112229,60990,60989,60997,60975,56550,60998],"class_list":["post-215","post","type-post","status-publish","format-standard","hentry","category-actividad-sismica","tag-actividad-sismica","tag-fallas-geologicas","tag-fallas-tectonicas","tag-rift-de-baikal","tag-sismicidad","tag-sismos","tag-zona-sismica"],"acf":[],"_links":{"self":[{"href":"https:\/\/sites.ipleiria.pt\/seismicknowledge\/wp-json\/wp\/v2\/posts\/215","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sites.ipleiria.pt\/seismicknowledge\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/sites.ipleiria.pt\/seismicknowledge\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/sites.ipleiria.pt\/seismicknowledge\/wp-json\/wp\/v2\/users\/3142"}],"replies":[{"embeddable":true,"href":"https:\/\/sites.ipleiria.pt\/seismicknowledge\/wp-json\/wp\/v2\/comments?post=215"}],"version-history":[{"count":1,"href":"https:\/\/sites.ipleiria.pt\/seismicknowledge\/wp-json\/wp\/v2\/posts\/215\/revisions"}],"predecessor-version":[{"id":217,"href":"https:\/\/sites.ipleiria.pt\/seismicknowledge\/wp-json\/wp\/v2\/posts\/215\/revisions\/217"}],"wp:attachment":[{"href":"https:\/\/sites.ipleiria.pt\/seismicknowledge\/wp-json\/wp\/v2\/media?parent=215"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/sites.ipleiria.pt\/seismicknowledge\/wp-json\/wp\/v2\/categories?post=215"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/sites.ipleiria.pt\/seismicknowledge\/wp-json\/wp\/v2\/tags?post=215"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}