{"id":11551,"date":"2021-07-14T19:43:43","date_gmt":"2021-07-14T17:43:43","guid":{"rendered":"http:\/\/volcanx.cluster031.hosting.ovh.net\/?page_id=11551"},"modified":"2021-10-04T18:34:43","modified_gmt":"2021-10-04T16:34:43","slug":"terremotos","status":"publish","type":"page","link":"https:\/\/volcanofoundation.org\/es\/creando-conocimiento-de-los-riesgos\/monitorizacion\/terremotos\/","title":{"rendered":"TERREMOTOS"},"content":{"rendered":"<div id=\"av_section_1\" class=\"avia-section av-av_section-a3505495476c97acb77226663f388d50 main_color avia-section-default avia-no-border-styling  avia-builder-el-0  el_before_av_section  avia-builder-el-first  avia-full-stretch av-parallax-section avia-bg-style-parallax av-minimum-height av-minimum-height-25 av-height-25  container_wrap fullsize\" data-section-bg-repeat=\"stretch\" data-av_minimum_height_pc=\"25\" data-av_min_height_opt=\"25\"><div class=\"av-parallax\" data-avia-parallax-ratio=\"0.3\"><div class=\"av-parallax-inner main_color avia-full-stretch\"><\/div><\/div><div class=\"container av-section-cont-open\"><main role=\"main\" itemprop=\"mainContentOfPage\" class=\"template-page content  av-content-full alpha units\"><div class=\"post-entry post-entry-type-page post-entry-11551\"><div class=\"entry-content-wrapper clearfix\">\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-av_one_fifth-25347b0a799d5b9f7058434b2a9c3182\">\n.flex_column.av-av_one_fifth-25347b0a799d5b9f7058434b2a9c3182{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-av_one_fifth-25347b0a799d5b9f7058434b2a9c3182 av_one_fifth  avia-builder-el-1  el_before_av_three_fifth  avia-builder-el-first  first flex_column_div av-zero-column-padding  \"><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-av_three_fifth-f7c1061df29de8cca6b42fcf455fe4a0\">\n.flex_column.av-av_three_fifth-f7c1061df29de8cca6b42fcf455fe4a0{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-av_three_fifth-f7c1061df29de8cca6b42fcf455fe4a0 av_three_fifth  avia-builder-el-2  el_after_av_one_fifth  el_before_av_one_fifth  flex_column_div av-zero-column-padding  \"><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-av_textblock-8d09e837ca2380e6bdc85d849f6641d9\">\n#top .av_textblock_section.av-av_textblock-8d09e837ca2380e6bdc85d849f6641d9 .avia_textblock{\ncolor:#ffffff;\n}\n<\/style>\n<section class=\"av_textblock_section av-av_textblock-8d09e837ca2380e6bdc85d849f6641d9 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock av_inherit_color\" itemprop=\"text\"><div class=\"h2-cinta-programas\">\n<h1 style=\"text-align: center; font-size: 2.5em;\">CREAR CONOCIMIENTO DE LOS RIESGOS<\/h1>\n<\/div>\n<\/div><\/section><br>\n<section class=\"av_textblock_section av-av_textblock-820f97e5aca1e77a0a12cd8a6430c9f2 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p class=\"p-cinta-programas\" style=\"text-align: center; background: #f5312a !important;\">&iquest;POR QU&Eacute; NACI&Oacute; LA FUNDACI&Oacute;N?<span class=\"flecha-donativo\" style=\"vertical-align: inherit;\"> &gt;<\/span><\/p>\n<\/div><\/section><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-av_one_fifth-f7c1061df29de8cca6b42fcf455fe4a0\">\n.flex_column.av-av_one_fifth-f7c1061df29de8cca6b42fcf455fe4a0{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-av_one_fifth-f7c1061df29de8cca6b42fcf455fe4a0 av_one_fifth  avia-builder-el-5  el_after_av_three_fifth  avia-builder-el-last  flex_column_div av-zero-column-padding  \"><\/div>\n\n<\/div><\/div><\/main><!-- close content main element --><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-k3yaxsym-b831a12c8acddceb21a18cbb360fd41d\">\n.avia-section.av-k3yaxsym-b831a12c8acddceb21a18cbb360fd41d{\nbackground-color:#000000;\nbackground-image:unset;\n}\n.avia-section.av-k3yaxsym-b831a12c8acddceb21a18cbb360fd41d .av-section-color-overlay{\nopacity:0.9;\nbackground-color:#000000;\n}\n<\/style>\n<div id=\"av_section_2\" class=\"avia-section av-k3yaxsym-b831a12c8acddceb21a18cbb360fd41d main_color avia-section-default avia-no-border-styling  avia-builder-el-6  el_after_av_section  el_before_av_textblock  avia-bg-style-fixed av-section-color-overlay-active container_wrap fullsize\"><div class=\"av-section-color-overlay-wrap\"><div class=\"av-section-color-overlay\"><\/div><div class=\"container av-section-cont-open\"><div class=\"template-page content  av-content-full alpha units\"><div class=\"post-entry post-entry-type-page post-entry-11551\"><div class=\"entry-content-wrapper clearfix\">\n<div class=\"flex_column_table av-a5p0bb-0286912bb6bfb93801b9fa33860921b2 sc-av_one_full av-equal-height-column-flextable\">\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-a5p0bb-0286912bb6bfb93801b9fa33860921b2\">\n.flex_column.av-a5p0bb-0286912bb6bfb93801b9fa33860921b2{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-a5p0bb-0286912bb6bfb93801b9fa33860921b2 av_one_full  avia-builder-el-7  avia-builder-el-no-sibling  first flex_column_table_cell av-equal-height-column av-align-middle av-zero-column-padding  \"><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-joihkone-69e81b3ac324ed7c1268b0d71e700013\">\n#top .av_textblock_section.av-joihkone-69e81b3ac324ed7c1268b0d71e700013 .avia_textblock{\nfont-size:18px;\ncolor:#ffffff;\n}\n\n@media only screen and (min-width: 768px) and (max-width: 989px){ \n#top .av_textblock_section.av-joihkone-69e81b3ac324ed7c1268b0d71e700013 .avia_textblock{\nfont-size:16px;\n}\n}\n\n@media only screen and (min-width: 480px) and (max-width: 767px){ \n#top .av_textblock_section.av-joihkone-69e81b3ac324ed7c1268b0d71e700013 .avia_textblock{\nfont-size:16px;\n}\n}\n\n@media only screen and (max-width: 479px){ \n#top .av_textblock_section.av-joihkone-69e81b3ac324ed7c1268b0d71e700013 .avia_textblock{\nfont-size:16px;\n}\n}\n<\/style>\n<section class=\"av_textblock_section av-joihkone-69e81b3ac324ed7c1268b0d71e700013 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock av_inherit_color\" itemprop=\"text\"><blockquote>\n<p><a href=\"http:\/\/www.undrr.org\"><strong>Los desastres no son naturales<\/strong><\/a>, se construyen socialmente, por falta de preparaci&oacute;n, prevenci&oacute;n, trabajo de mitigaci&oacute;n, educaci&oacute;n y vigilancia. Son riesgos o peligros naturales que impactan en las sociedades vulnerables. El conocimiento ayuda a <strong>reducir la vulnerabilidad social<\/strong> y <strong>estructural<\/strong> para tener sociedades m&aacute;s <strong>resilientes<\/strong>!<\/p>\n<\/blockquote>\n<\/div><\/section><\/div><\/div><!--close column table wrapper. Autoclose: 1 -->\n<\/div><\/div><\/div><!-- close content main div --><\/div><\/div><\/div><div id=\"after_section_2\" class=\"main_color av_default_container_wrap container_wrap fullsize\"><div class=\"container av-section-cont-open\"><div class=\"template-page content  av-content-full alpha units\"><div class=\"post-entry post-entry-type-page post-entry-11551\"><div class=\"entry-content-wrapper clearfix\">\n<section class=\"av_textblock_section av-kqt9jd5e-cd33964ef4e3b772df7fef522b816d29 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><h2>El seguimiento de la sismicidad de los volcanes ayuda a <a href=\"http:\/\/www.undrr.org\">comprender<\/a> la estructura de los volcanes<\/h2>\n<\/div><\/section>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-kqt9ln1w-f6affe7cdeee6be02fc225bbc4bc5689\">\n#top .hr.av-kqt9ln1w-f6affe7cdeee6be02fc225bbc4bc5689{\nmargin-top:15px;\nmargin-bottom:15px;\n}\n.hr.av-kqt9ln1w-f6affe7cdeee6be02fc225bbc4bc5689 .hr-inner{\nwidth:100%;\nborder-color:#d8d8d8;\n}\n<\/style>\n<div class=\"hr av-kqt9ln1w-f6affe7cdeee6be02fc225bbc4bc5689 hr-custom  avia-builder-el-10  el_after_av_textblock  el_before_av_three_fifth  hr-center hr-icon-no\"><span class=\"hr-inner inner-border-av-border-thin\"><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-1wlhzr6-8cc129343b9618e21784b665a1361b31\">\n.flex_column.av-1wlhzr6-8cc129343b9618e21784b665a1361b31{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-1wlhzr6-8cc129343b9618e21784b665a1361b31 av_three_fifth  avia-builder-el-11  el_after_av_hr  el_before_av_two_fifth  first flex_column_div av-zero-column-padding  \"><section class=\"av_textblock_section av-kqt9tgn4-955ae44a3b12f5f76d41e08b4c147261 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><h3>El magma en movimiento y los fluidos volc&aacute;nicos provocan terremotos<\/h3>\n<p>Muchos procesos pueden generar <strong>terremotos en terrenos volc&aacute;nicos<\/strong>. La mayor&iacute;a de las veces, estos procesos son fallas y fracturas que no necesariamente conducen a una erupci&oacute;n. <strong>Los terremotos volc&aacute;nicos<\/strong> se producen cuando el <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;MAGMA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Roca fundida bajo la superficie de la Tierra.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/magma-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>magma<\/a> y los gases volc&aacute;nicos suben a la superficie desde las profundidades del subsuelo, lo que implica grandes cambios de tensi&oacute;n en la <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;CORTEZA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;La corteza es la capa principal m&aacute;s externa de la tierra, que oscila entre unos 10 y 65 km de espesor en todo el mundo. Los 15-35 km m&aacute;s altos de corteza son lo suficientemente fr&aacute;giles como para producir terremotos.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/corteza-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>corteza<\/a> a medida que el material migra hacia arriba.<\/p>\n<\/div><\/section><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-kqta1i5b-a345f9d882c51d4089993cf6d16e9b60\">\n#top .hr.hr-invisible.av-kqta1i5b-a345f9d882c51d4089993cf6d16e9b60{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-kqta1i5b-a345f9d882c51d4089993cf6d16e9b60 hr-invisible  avia-builder-el-13  el_after_av_textblock  el_before_av_textblock \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div><br>\n<section class=\"av_textblock_section av-kqtdsfvd-d152eb0e3d3e094fcc403a1e69a26b44 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><h3><a title=\"EL 60% DE LOS VOLCANES ACTIVOS NO TIENEN SISTEMA DE MONITORIZACI&Oacute;N\" href=\"http:\/\/volcanx.cluster031.hosting.ovh.net\/most-of-active-volcanoes-have-no-monitoring-system\/\">Los sism&oacute;logos de los volcanes estudian<\/a> varios tipos de eventos s&iacute;smicos para entender mejor c&oacute;mo se mueven el magma y los gases hacia la superficie:<\/h3>\n<\/div><\/section><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-1auxuce-446d26f09781275ead180812c8c73cd6\">\n#top .hr.hr-invisible.av-1auxuce-446d26f09781275ead180812c8c73cd6{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-1auxuce-446d26f09781275ead180812c8c73cd6 hr-invisible  avia-builder-el-15  el_after_av_textblock  el_before_av_textblock \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div><br>\n<section class=\"av_textblock_section av-kqtdv7q3-ddccd14f13f4a7f2a8db2af689b19cc8 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p><strong>Las redes de vigilancia s&iacute;smica<\/strong> de los volcanes son muy heterog&eacute;neas entre pa&iacute;ses y volcanes. Los terremotos volc&aacute;nicos se producen cuando el <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;MAGMA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Roca fundida bajo la superficie de la Tierra.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/magma-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>magma<\/a> y los gases volc&aacute;nicos suben a la superficie desde las profundidades del subsuelo, lo que provoca grandes cambios de tensi&oacute;n en la <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;CORTEZA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;La corteza es la capa principal m&aacute;s externa de la tierra, que oscila entre unos 10 y 65 km de espesor en todo el mundo. Los 15-35 km m&aacute;s altos de corteza son lo suficientemente fr&aacute;giles como para producir terremotos.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/corteza-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>corteza<\/a>, ya que los terremotos volcanotect&oacute;nicos (VT) representan la fractura fr&aacute;gil de la roca, el mismo proceso que se produce a lo largo de las fallas puramente &laquo;tect&oacute;nicas&raquo;.<br>\n1-En los volcanes, los <strong>terremotos VT<\/strong> pueden producirse debido a fuerzas tect&oacute;nicas &laquo;normales&raquo;, a tensiones cambiantes causadas por el <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;MAGMA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Roca fundida bajo la superficie de la Tierra.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/magma-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>magma<\/a> en movimiento y al movimiento de fluidos a trav&eacute;s de grietas preexistentes. Distinguir entre estos diferentes procesos puede ser complicado y a menudo requiere datos de otras disciplinas (geodesia, <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;HIDROLOG&Iacute;A&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;La ciencia que abarca el comportamiento del agua tal como ocurre en la atm&oacute;sfera, en la superficie del suelo y bajo tierra.&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/hidrologia-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">hidrolog&iacute;a<\/a>, geoqu&iacute;mica de gases y geolog&iacute;a)<br>\n2- Los <strong>per&iacute;odos largos<\/strong> (LP) o <strong>baja frecuencia<\/strong> (LF) <strong>sismos terrestres<\/strong> son causados por grietas que resuenan cuando el <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;MAGMA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Roca fundida bajo la superficie de la Tierra.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/magma-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>magma<\/a> y los gases se mueven hacia la superficie. A menudo se observan antes de las erupciones volc&aacute;nicas, pero su aparici&oacute;n tambi&eacute;n forma parte de la sismicidad de fondo normal de algunos volcanes y su aparici&oacute;n no indica necesariamente que una erupci&oacute;n sea inminente. Los eventos LF tambi&eacute;n pueden ser producidos por procesos no magm&aacute;ticos, incluyendo el movimiento de los glaciares.<br>\n3- <strong>El tremor<\/strong> es una se&ntilde;al s&iacute;smica continua de gran amplitud que puede ser causada por m&uacute;ltiples procesos, incluyendo la resonancia de larga duraci&oacute;n debida al movimiento prolongado del <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;MAGMA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Roca fundida bajo la superficie de la Tierra.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/magma-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>magma<\/a> a trav&eacute;s de las fisuras, la ocurrencia continua de eventos VT o LP\/LF que est&aacute;n tan pr&oacute;ximos en el tiempo que no pueden ser separados visualmente, y las explosiones.<br>\n4- Los conjuntos s&iacute;smicos de superficie pueden ser par&aacute;sitos o &uacute;tiles para la vigilancia. Las fuentes pueden ser antropog&eacute;nicas, desprendimientos de rocas, terremotos de hielo, deslizamientos de tierra, flujos pirocl&aacute;sticos y lahares, explosiones.<\/p>\n<\/div><\/section><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-280wm6-7143270a863b5edf6aeeb91449c82f9d\">\n#top .hr.hr-invisible.av-280wm6-7143270a863b5edf6aeeb91449c82f9d{\nheight:10px;\n}\n<\/style>\n<div class=\"hr av-280wm6-7143270a863b5edf6aeeb91449c82f9d hr-invisible  avia-builder-el-17  el_after_av_textblock  el_before_av_textblock \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div><br>\n<section class=\"av_textblock_section av-kqtdvi1g-d58b1510582040230a4a9aa8e33ee63c \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p><strong><a title=\"BUILDING RISK KNOWLEDGE\" href=\"http:\/\/volcanx.cluster031.hosting.ovh.net\/building-risk-knowledge\/\">La mayor&iacute;a de los terremotos relacionados con los volcanes<\/a> son demasiado peque&ntilde;os para sentirlos<\/strong>, generalmente bastante superficiales (normalmente a menos de 10 km (7 mi) de la superficie), y pueden ocurrir en enjambres que consisten en docenas o cientos de eventos. La mayor&iacute;a de los enjambres no suelen provocar erupciones, pero la mayor&iacute;a de las erupciones van precedidas de enjambres. Por lo tanto, durante los per&iacute;odos de mayor actividad s&iacute;smica en un volc&aacute;n, los sism&oacute;logos trabajan las 24 horas del d&iacute;a para detectar variaciones sutiles en el tipo, la ubicaci&oacute;n y la intensidad de la actividad s&iacute;smica para determinar si puede producirse una erupci&oacute;n.<\/p>\n<\/div><\/section><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-1iz7j36-2c9786a9f3f90bd1396461500bfb925f\">\n.flex_column.av-1iz7j36-2c9786a9f3f90bd1396461500bfb925f{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-1iz7j36-2c9786a9f3f90bd1396461500bfb925f av_two_fifth  avia-builder-el-19  el_after_av_three_fifth  avia-builder-el-last  flex_column_div av-zero-column-padding  \"><p>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-kqtcpnnn-1475634e8484c98b100bb0d3be46e0a0\">\n.avia-image-container.av-kqtcpnnn-1475634e8484c98b100bb0d3be46e0a0 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-kqtcpnnn-1475634e8484c98b100bb0d3be46e0a0 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<\/p><div class=\"avia-image-container av-kqtcpnnn-1475634e8484c98b100bb0d3be46e0a0 av-styling- avia-align-center  avia-builder-el-20  el_before_av_textblock  avia-builder-el-first \" itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\"><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><img decoding=\"async\" fetchpriority=\"high\" class=\"wp-image-11558 avia-img-lazy-loading-not-11558 avia_image \" src=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/seismogrm-signal-volcanic-earthquakes.png\" alt=\"\" title=\"seismogrm-signal-volcanic-earthquakes\" height=\"1190\" width=\"1140\" itemprop=\"thumbnailUrl\" srcset=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/seismogrm-signal-volcanic-earthquakes.png 1140w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/seismogrm-signal-volcanic-earthquakes-287x300.png 287w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/seismogrm-signal-volcanic-earthquakes-987x1030.png 987w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/seismogrm-signal-volcanic-earthquakes-768x802.png 768w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/seismogrm-signal-volcanic-earthquakes-675x705.png 675w\" sizes=\"(max-width: 1140px) 100vw, 1140px\"\/><\/div><\/div><\/div><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-kqtcpuh7-d8db4528b4900c045b62972c54904769\">\n#top .av_textblock_section.av-kqtcpuh7-d8db4528b4900c045b62972c54904769 .avia_textblock{\nfont-size:14px;\n}\n<\/style>\n<section class=\"av_textblock_section av-kqtcpuh7-d8db4528b4900c045b62972c54904769 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p><em>Ejemplos de se&ntilde;ales de sismos volc&aacute;nicos: volcano <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;TECT&Oacute;NICO&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Relativo a la deformaci&oacute;n estructural de la corteza terrestre.&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/tectonico-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">tect&oacute;nico<\/a> (VT), baja frecuencia (LF)\/largo per&iacute;odo profundo (DLP), h&iacute;brido (mezcla de VT y LF), muy baja frecuencia (VLF) y temblor.<\/em><\/p>\n<\/div><\/section><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-14hay76-b9bade6c53b94b7d00ae79f4a86820fd\">\n#top .hr.hr-invisible.av-14hay76-b9bade6c53b94b7d00ae79f4a86820fd{\nheight:30px;\n}\n<\/style>\n<div class=\"hr av-14hay76-b9bade6c53b94b7d00ae79f4a86820fd hr-invisible  avia-builder-el-22  el_after_av_textblock  avia-builder-el-last \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div><\/div>\n<\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>The seismic sources of volcanoes are varied and complex. They involve interactions between <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;MAGMA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Roca fundida bajo la superficie de la Tierra.&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/magma-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">magma<\/a>, gaseous or liquid fluids and solids. These specialities make volcanic seismology a science in its own right.<\/p>\n","protected":false},"author":8,"featured_media":10113,"parent":11395,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-11551","page","type-page","status-publish","has-post-thumbnail","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/pages\/11551","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/users\/8"}],"replies":[{"embeddable":true,"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/comments?post=11551"}],"version-history":[{"count":0,"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/pages\/11551\/revisions"}],"up":[{"embeddable":true,"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/pages\/11395"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/media\/10113"}],"wp:attachment":[{"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/media?parent=11551"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}