{"id":12743,"date":"2021-07-21T16:38:55","date_gmt":"2021-07-21T14:38:55","guid":{"rendered":"http:\/\/volcanx.cluster031.hosting.ovh.net\/?page_id=12743"},"modified":"2021-10-04T18:39:29","modified_gmt":"2021-10-04T16:39:29","slug":"corrientes-de-densidad-piroclastica","status":"publish","type":"page","link":"https:\/\/volcanofoundation.org\/es\/creando-conocimiento-de-los-riesgos\/peligros\/corrientes-de-densidad-piroclastica\/","title":{"rendered":"CORRIENTES DE DENSIDAD PIROCL\u00c1STICA"},"content":{"rendered":"<div id=\"av_section_1\" class=\"avia-section av-85tvrm-3e95231a7b3e6eb192907f404f41a286 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-12743\"><div class=\"entry-content-wrapper clearfix\">\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-377mki-891bdcf97286948f143384db57d78c91\">\n.flex_column.av-377mki-891bdcf97286948f143384db57d78c91{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-377mki-891bdcf97286948f143384db57d78c91 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-44v1oi-4270c45783cf4dfabc2e0046b5bfca7a\">\n.flex_column.av-44v1oi-4270c45783cf4dfabc2e0046b5bfca7a{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-44v1oi-4270c45783cf4dfabc2e0046b5bfca7a 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-2wneaq-c7141c0f93804d3dc6134a419c02967d\">\n#top .av_textblock_section.av-2wneaq-c7141c0f93804d3dc6134a419c02967d .avia_textblock{\ncolor:#ffffff;\n}\n<\/style>\n<section class=\"av_textblock_section av-2wneaq-c7141c0f93804d3dc6134a419c02967d \" 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-2wneaq-34462baf835e0e88628f9f1fcf41a06e \" 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-377mki-fc3240a24cacc3f72868647236f26abd\">\n.flex_column.av-377mki-fc3240a24cacc3f72868647236f26abd{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-377mki-fc3240a24cacc3f72868647236f26abd 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_one_full  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-12743\"><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-12743\"><div class=\"entry-content-wrapper clearfix\">\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-36ozj7x-f03a033a1217e5355e0203f5fe196b40\">\n.flex_column.av-36ozj7x-f03a033a1217e5355e0203f5fe196b40{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-36ozj7x-f03a033a1217e5355e0203f5fe196b40 av_one_full  avia-builder-el-9  el_after_av_section  el_before_av_one_half  avia-builder-el-first  first flex_column_div av-zero-column-padding  \"><section class=\"av_textblock_section av-kqt9jd5e-cd33964ef4e3b772df7fef522b816d29 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><h2>Los flujos pirocl&aacute;sticos se mueven r&aacute;pidamente y destruyen todo a su paso<\/h2>\n<p>.<br>\nPreste atenci&oacute;n a las advertencias de evacuaci&oacute;n si se sabe que un volc&aacute;n est&aacute; activo. Si eres testigo de un <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;FLUJO PIROCL&Aacute;STICO&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;Una mezcla caliente (t&iacute;picamente &amp;amp;gt;800 &deg;C), ca&oacute;tica de fragmentos de roca, gas y cenizas que viaja r&aacute;pidamente (decenas de metros por segundo) lejos de un respiradero volc&aacute;nico o frente de flujo colapsante.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/flujo-piroclastico-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">flujo pirocl&aacute;stico<\/a>, corre en direcci&oacute;n contraria lo m&aacute;s r&aacute;pido posible.<\/p>\n<hr>\n<p>Los flujos pirocl&aacute;sticos contienen una mezcla de alta densidad de bloques de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;T&eacute;rmino general para magma (roca moldeada) que ha entrado en erupci&oacute;n en la superficie de la Tierra y mantiene su integridad como una masa fluida o viscosa, en lugar de explotar en fragmentos.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/lava-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lava<\/a> caliente, piedra <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;P&Oacute;MEZ&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Eyecci&oacute;n volc&aacute;nica altamente vesicular, t&iacute;picamente sil&iacute;cica en composici&oacute;n. Es esencialmente magma que ha sido espumado por gases escapando y luego enfriado y solidificado durante la erupci&oacute;n. La piedra p&oacute;mez riol&iacute;tica es t&iacute;picamente de densidad lo suficientemente baja como para flotar en el agua. Cerca de un respiradero, la piedra p&oacute;mez caliente puede acumularse y formar un cono de piedra p&oacute;mez.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/pomez-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>p&oacute;mez<\/a>, <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;CENIZA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Fragmentos finos (de menos de 2-4 mm de di&aacute;metro) de roca volc&aacute;nica formados por una explosi&oacute;n volc&aacute;nica o por la eyecci&oacute;n de una chimenea volc&aacute;nica.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/ceniza-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>ceniza<\/a> y gas <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;VOLC&Aacute;NICO&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;Cuerpo de roca que se compone de fragmentos de rocas o minerales derivados volc&aacute;nicamente que luego fueron transportados a cierta distancia de su lugar de origen.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/volcanico-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">volc&aacute;nico<\/a>. Se desplazan a gran velocidad por las laderas volc&aacute;nicas, normalmente siguiendo los valles. La mayor&iacute;a de los flujos pirocl&aacute;sticos constan de dos partes: un flujo inferior (basal) de fragmentos gruesos que se desplaza por el suelo, y una nube turbulenta de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;CENIZA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Fragmentos finos (de menos de 2-4 mm de di&aacute;metro) de roca volc&aacute;nica formados por una explosi&oacute;n volc&aacute;nica o por la eyecci&oacute;n de una chimenea volc&aacute;nica.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/ceniza-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>ceniza<\/a> que se eleva por encima del flujo basal. La <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;CENIZA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Fragmentos finos (de menos de 2-4 mm de di&aacute;metro) de roca volc&aacute;nica formados por una explosi&oacute;n volc&aacute;nica o por la eyecci&oacute;n de una chimenea volc&aacute;nica.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/ceniza-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>ceniza<\/a> puede caer desde esta nube en una amplia zona a favor del viento desde el <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;FLUJO PIROCL&Aacute;STICO&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;Una mezcla caliente (t&iacute;picamente &amp;amp;gt;800 &deg;C), ca&oacute;tica de fragmentos de roca, gas y cenizas que viaja r&aacute;pidamente (decenas de metros por segundo) lejos de un respiradero volc&aacute;nico o frente de flujo colapsante.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/flujo-piroclastico-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">flujo pirocl&aacute;stico<\/a>.<\/p>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-2oox78t-7b8ceff52f6c37aeb4bff6691ec462f6\">\n#top .hr.hr-invisible.av-2oox78t-7b8ceff52f6c37aeb4bff6691ec462f6{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-2oox78t-7b8ceff52f6c37aeb4bff6691ec462f6 hr-invisible  avia-builder-el-11  el_before_av_hr  avia-builder-el-first \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n<p>Los flujos pirocl&aacute;sticos se forman de diferentes maneras:<\/p>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-25khogd-d35e89b526de08b32933e0391fc1ee90\">\n#top .hr.hr-invisible.av-25khogd-d35e89b526de08b32933e0391fc1ee90{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-25khogd-d35e89b526de08b32933e0391fc1ee90 hr-invisible  avia-builder-el-12  el_after_av_hr  avia-builder-el-last \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n<ul>\n<li>Colapso de la <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;COLUMNA DE ERUPCI&Oacute;N&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;La parte vertical ascendente de la masa de escombros y gas volc&aacute;nico en erupci&oacute;n que se eleva directamente sobre una chimenea volc&aacute;nica. M&aacute;s arriba en la atm&oacute;sfera, las columnas suelen extenderse lateralmente en penachos o nubes paraguas.&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/columna-erupcion-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">columna de erupci&oacute;n<\/a>: durante una erupci&oacute;n altamente explosiva, la columna expulsada hacia arriba en la atm&oacute;sfera se enfr&iacute;a y puede llegar a ser demasiado fr&iacute;a y densa para mantener el impulso ascendente.<\/li>\n<li>&laquo;Hervidero&raquo; del respiradero eruptivo: durante una <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;ERUPCI&Oacute;N EXPLOSIVA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;An energetic eruption that produces mainly ash, pumice, and fragmental ballistic debris (as opposed to an effusive eruption).&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/erupcion-explosiva-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">erupci&oacute;n explosiva<\/a>, el material sale sin formar un penacho alto y se desplaza r&aacute;pidamente ladera abajo.<\/li>\n<li>Colapso de domos o flujos de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;T&eacute;rmino general para magma (roca moldeada) que ha entrado en erupci&oacute;n en la superficie de la Tierra y mantiene su integridad como una masa fluida o viscosa, en lugar de explotar en fragmentos.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/lava-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lava<\/a>: Los frentes de los flujos o domos de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;T&eacute;rmino general para magma (roca moldeada) que ha entrado en erupci&oacute;n en la superficie de la Tierra y mantiene su integridad como una masa fluida o viscosa, en lugar de explotar en fragmentos.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/lava-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lava<\/a> pueden llegar a ser tan empinados que se colapsan debido a la fuerza gravitacional.<\/li>\n<li>\n<\/li><\/ul>\n<h3>Los flujos pirocl&aacute;sticos destruyen casi todo a su paso<\/h3>\n<p>Con fragmentos de roca que var&iacute;an en tama&ntilde;o, desde cenizas hasta rocas, que se desplazan por el suelo a velocidades normalmente superiores a los 80 km por hora (50 mph), los flujos pirocl&aacute;sticos derriban, destrozan, entierran o arrastran casi todos los objetos y estructuras a su paso. Las temperaturas extremas de las rocas y el gas en el interior de los flujos pirocl&aacute;sticos, generalmente entre 200&deg;C y 700&deg;C (390-1300&deg;F), pueden encender incendios y derretir la nieve y el hielo.<\/p>\n<\/div><\/section><\/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_one_half  avia-builder-el-13  el_after_av_one_full  el_before_av_one_half  first flex_column_div av-zero-column-padding  column-top-margin\"><p><section class=\"av_textblock_section av-kqt9tgn4-955ae44a3b12f5f76d41e08b4c147261 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p>Los flujos pirocl&aacute;sticos var&iacute;an considerablemente en tama&ntilde;o y velocidad, pero incluso los flujos relativamente peque&ntilde;os que se desplazan a menos de 5 km (3 mi) de un volc&aacute;n pueden destruir edificios, bosques y tierras de cultivo. En los m&aacute;rgenes de los flujos pirocl&aacute;sticos, las personas y los animales pueden morir o sufrir lesiones graves por las quemaduras y la inhalaci&oacute;n de cenizas y gases calientes.<\/p>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-1ioqbv1-ab0657143c57a8b88771661a78b2d6bb\">\n#top .hr.hr-invisible.av-1ioqbv1-ab0657143c57a8b88771661a78b2d6bb{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-1ioqbv1-ab0657143c57a8b88771661a78b2d6bb hr-invisible  avia-builder-el-15  el_before_av_hr  avia-builder-el-first \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n<p>Los flujos pirocl&aacute;sticos generalmente siguen los valles u otras zonas bajas y, dependiendo del volumen de los restos de roca arrastrados por el flujo, pueden depositar capas de fragmentos de roca sueltos a profundidades que van desde menos de un metro hasta m&aacute;s de 200 m (hasta unos 700 pies).<\/p>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-19fz5v1-a2937d67951683001963c767859a1470\">\n#top .hr.hr-invisible.av-19fz5v1-a2937d67951683001963c767859a1470{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-19fz5v1-a2937d67951683001963c767859a1470 hr-invisible  avia-builder-el-16  el_after_av_hr  el_before_av_hr \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n<p>Los flujos pirocl&aacute;sticos tambi&eacute;n pueden provocar peligros secundarios, especialmente inundaciones y lahares:<\/p>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-n9n0st-0df5ad731993668311d90ed04620e1df\">\n#top .hr.hr-invisible.av-n9n0st-0df5ad731993668311d90ed04620e1df{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-n9n0st-0df5ad731993668311d90ed04620e1df hr-invisible  avia-builder-el-17  el_after_av_hr  avia-builder-el-last \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n<ul>\n<li>Deshielo, fusi&oacute;n y mezcla con la nieve y el hielo, enviando as&iacute; un torrente repentino r&iacute;o abajo.<\/li>\n<li>Por ejemplo, la construcci&oacute;n de una casa de campo.<\/li>\n<li>El bloqueo de los arroyos en los valles volc&aacute;nicos, lo que puede crear lagos detr&aacute;s de la obstrucci&oacute;n que eventualmente se desbordan y erosionan la obstrucci&oacute;n produciendo un torrente de agua y material <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;VOLC&Aacute;NICO&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;Cuerpo de roca que se compone de fragmentos de rocas o minerales derivados volc&aacute;nicamente que luego fueron transportados a cierta distancia de su lugar de origen.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/volcanico-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">volc&aacute;nico<\/a> aguas abajo.<\/li>\n<li>La reducci&oacute;n de la velocidad de los arroyos en los valles volc&aacute;nicos.<\/li>\n<li>Aumentar la tasa de escorrent&iacute;a de los arroyos y la erosi&oacute;n durante las tormentas de lluvia debido a la creaci&oacute;n de un paisaje f&aacute;cilmente erosionable con escasa vegetaci&oacute;n.<\/li>\n<\/ul>\n<\/div><\/section><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-kqta1i5b-107d1a9c40127944f7fe3b907c4f1f41\">\n#top .hr.hr-invisible.av-kqta1i5b-107d1a9c40127944f7fe3b907c4f1f41{\nheight:30px;\n}\n<\/style>\n<\/p><div class=\"hr av-kqta1i5b-107d1a9c40127944f7fe3b907c4f1f41 hr-invisible  avia-builder-el-18  el_after_av_textblock  avia-builder-el-last \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-4syb7u1-2e782103a5a11106f5050bb03ca2c081\">\n.flex_column.av-4syb7u1-2e782103a5a11106f5050bb03ca2c081{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-4syb7u1-2e782103a5a11106f5050bb03ca2c081 av_one_half  avia-builder-el-19  el_after_av_one_half  el_before_av_one_full  flex_column_div av-zero-column-padding  column-top-margin\"><p>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-kr6ib1mz-969b8b168ca22ea734c7b8b660ca0e13\">\n.avia-image-container.av-kr6ib1mz-969b8b168ca22ea734c7b8b660ca0e13 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-kr6ib1mz-969b8b168ca22ea734c7b8b660ca0e13 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<\/p><div class=\"avia-image-container av-kr6ib1mz-969b8b168ca22ea734c7b8b660ca0e13 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-12728 avia-img-lazy-loading-not-12728 avia_image \" src=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/building-remnant-francisco-leon-destroyed.jpg\" alt=\"\" title=\"building-remnant-francisco-leon-destroyed\" height=\"500\" width=\"800\" itemprop=\"thumbnailUrl\" srcset=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/building-remnant-francisco-leon-destroyed.jpg 800w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/building-remnant-francisco-leon-destroyed-300x188.jpg 300w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/building-remnant-francisco-leon-destroyed-768x480.jpg 768w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/building-remnant-francisco-leon-destroyed-705x441.jpg 705w\" sizes=\"(max-width: 800px) 100vw, 800px\"\/><\/div><\/div><\/div><br>\n<section class=\"av_textblock_section av-kr6i76jb-4d99ac4ff95732f9d5a32379964de404 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p style=\"text-align: right;\"><em>Restos de edificios en Francisco Le&oacute;n destruidos por oleadas y flujos pirocl&aacute;sticos durante la erupci&oacute;n del volc&aacute;n El Chich&oacute;n en M&eacute;xico 1982. Las varillas de refuerzo en el concreto se doblan en la direcci&oacute;n del flujo.<\/em><\/p>\n<\/div><\/section><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-4b7podl-d558ccf1b9e3dec760b5573ff0ebb60d\">\n#top .hr.hr-invisible.av-4b7podl-d558ccf1b9e3dec760b5573ff0ebb60d{\nheight:30px;\n}\n<\/style>\n<div class=\"hr av-4b7podl-d558ccf1b9e3dec760b5573ff0ebb60d 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<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-sodwq8-5ae05c90d4a40f1187f37c8f84f0c3f3\">\n.flex_column.av-sodwq8-5ae05c90d4a40f1187f37c8f84f0c3f3{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-sodwq8-5ae05c90d4a40f1187f37c8f84f0c3f3 av_one_full  avia-builder-el-23  el_after_av_one_half  el_before_av_one_full  first flex_column_div av-zero-column-padding  column-top-margin\"><section class=\"av_textblock_section av-kr6lajxb-0d3a9ea424224b6152a6f95282938c7e \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p>Las estimaciones cient&iacute;ficas publicadas sobre la tasa de emisi&oacute;n global de CO2 de todos los volcanes suba&eacute;reos (en tierra) y submarinos que desgasifican se sit&uacute;an en un rango de 0,13 gigatoneladas a 0,44 gigatoneladas por a&ntilde;o. La emisi&oacute;n antropog&eacute;nica de CO2 de 35 gigatones prevista para 2010 es entre 80 y 270 veces mayor que las respectivas estimaciones de emisi&oacute;n volc&aacute;nica mundial m&aacute;xima y m&iacute;nima.<\/p>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-648igr-b096078d1b4b82208a3cc2b0b683083d\">\n#top .hr.hr-invisible.av-648igr-b096078d1b4b82208a3cc2b0b683083d{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-648igr-b096078d1b4b82208a3cc2b0b683083d hr-invisible  avia-builder-el-25  el_before_av_hr  avia-builder-el-first \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n<p>No hay duda de que las grandes erupciones volc&aacute;nicas pueden inyectar cantidades significativas de di&oacute;xido de carbono en la atm&oacute;sfera. La erupci&oacute;n del Monte Santa Helena en 1980 expuls&oacute; a la atm&oacute;sfera aproximadamente 10 millones de toneladas de CO2 en s&oacute;lo 9 horas. Sin embargo, actualmente la humanidad s&oacute;lo tarda 2,5 horas en expulsar la misma cantidad. Mientras que las grandes erupciones explosivas como &eacute;sta son raras y s&oacute;lo ocurren globalmente cada 10 a&ntilde;os aproximadamente, las <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;EMISIONES&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;La liberaci&oacute;n de gases volc&aacute;nicos de la tierra, que escapan a la atm&oacute;sfera.&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/emisiones-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">emisiones<\/a> de la humanidad son incesantes y aumentan cada a&ntilde;o.<\/p>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-151wkqj-9bbe1dd91e9014edd45c994d4872c2b3\">\n#top .hr.hr-invisible.av-151wkqj-9bbe1dd91e9014edd45c994d4872c2b3{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-151wkqj-9bbe1dd91e9014edd45c994d4872c2b3 hr-invisible  avia-builder-el-26  el_after_av_hr  el_before_av_hr \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n<p>Se siguen realizando esfuerzos para reducir las incertidumbres y mejorar las estimaciones de las <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;EMISIONES&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;La liberaci&oacute;n de gases volc&aacute;nicos de la tierra, que escapan a la atm&oacute;sfera.&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/emisiones-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">emisiones<\/a> volc&aacute;nicas globales de CO2 en la actualidad, pero los cient&iacute;ficos especializados en gases volc&aacute;nicos tienen pocas dudas de que las <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;EMISIONES&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;La liberaci&oacute;n de gases volc&aacute;nicos de la tierra, que escapan a la atm&oacute;sfera.&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/emisiones-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">emisiones<\/a> antropog&eacute;nicas de CO2 empeque&ntilde;ecen las <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;EMISIONES&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;La liberaci&oacute;n de gases volc&aacute;nicos de la tierra, que escapan a la atm&oacute;sfera.&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/emisiones-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">emisiones<\/a> volc&aacute;nicas globales de CO2.<\/p>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-tqb7zv-9b53a6639a30a0e184c4fd1b76ccf8c3\">\n#top .hr.hr-invisible.av-tqb7zv-9b53a6639a30a0e184c4fd1b76ccf8c3{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-tqb7zv-9b53a6639a30a0e184c4fd1b76ccf8c3 hr-invisible  avia-builder-el-27  el_after_av_hr  avia-builder-el-last \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n<p>Para obtener informaci&oacute;n adicional sobre este tema, lea el art&iacute;culo de Eos de la Uni&oacute;n Geof&iacute;sica Americana &laquo;Volcanic Versus Anthropogenic Carbon Dioxide&raquo;, escrito por el cient&iacute;fico del USGS Terrence M. Gerlach.<\/p>\n<\/div><\/section><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-snwrg0-a0516b7754c224557f049603b3a431cb\">\n.flex_column.av-snwrg0-a0516b7754c224557f049603b3a431cb{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-snwrg0-a0516b7754c224557f049603b3a431cb av_one_full  avia-builder-el-28  el_after_av_one_full  avia-builder-el-last  first flex_column_div av-zero-column-padding  column-top-margin\"><section class=\"av_textblock_section av-kr6lc7kn-8447ba711fabcae21f6ed842284a9265 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><table class=\"table table-striped\" border=\"1\" cellpadding=\"2\">\n<tbody>\n<tr>\n<td><strong>Yearly CO<sub>2<\/sub>&nbsp;emitters<\/strong><\/td>\n<td><strong>Billion metric tons per year (Gt\/y)<\/strong><\/td>\n<\/tr>\n<tr>\n<td>Global volcanic emissions (highest preferred estimate)<\/td>\n<td>&nbsp;&nbsp;&nbsp;&nbsp;0.26<\/td>\n<\/tr>\n<tr>\n<td>Anthropogenic CO<sub>2<\/sub>&nbsp;from fuel combustion 2015<sup>+<\/sup><\/td>\n<td>32.3<\/td>\n<\/tr>\n<tr>\n<td>Worldwide Road Transportation 2015<sup>+<\/sup><\/td>\n<td>&nbsp;&nbsp;5.8<\/td>\n<\/tr>\n<tr>\n<td>Approximately 24 1000-megawatt coal-fired power stations&nbsp;*<\/td>\n<td>&nbsp;&nbsp;&nbsp;&nbsp;0.22<\/td>\n<\/tr>\n<tr>\n<td>Argentina 2015<sup>+<\/sup><\/td>\n<td>&nbsp;&nbsp;&nbsp;&nbsp;0.19<\/td>\n<\/tr>\n<tr>\n<td>Poland 2015<sup>+<\/sup><\/td>\n<td>&nbsp;&nbsp;&nbsp;&nbsp;0.28<\/td>\n<\/tr>\n<tr>\n<td>United States 2015<sup>+<\/sup><\/td>\n<td>&nbsp;&nbsp;&nbsp;&nbsp;4.99<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<\/div><\/section><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-zvbbqz-40ae4514aa60604ae2de2cf16ffbf33e\">\n#top .hr.hr-invisible.av-zvbbqz-40ae4514aa60604ae2de2cf16ffbf33e{\nheight:30px;\n}\n<\/style>\n<div class=\"hr av-zvbbqz-40ae4514aa60604ae2de2cf16ffbf33e hr-invisible  avia-builder-el-30  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-kr6ltla0-6ba6214b14e9dedb8b4ef33cf2021836 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><table class=\"table table-striped\" border=\"1\" cellpadding=\"2\">\n<tbody>\n<tr>\n<td><strong>CO<sub>2<\/sub>&nbsp;emission&nbsp;events<\/strong><\/td>\n<td><\/td>\n<\/tr>\n<tr>\n<td>Mount St. Helens, 18 May 1980<\/td>\n<td>0.01 Gt<\/td>\n<\/tr>\n<tr>\n<td>Mount Pinatubo, 15 June 1991<\/td>\n<td>0.05 Gt<\/td>\n<\/tr>\n<tr>\n<td>Number of Pinatubo-equivalent eruptions equal to 2010 global anthropogenic CO<sub>2<\/sub><\/td>\n<td>700<\/td>\n<\/tr>\n<tr>\n<td>Number of Mount St. Helens-equivalent eruptions equal to 2010 global anthropogenic CO<sub>2<\/sub><\/td>\n<td>3500<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<\/div><\/section><br>\n<section class=\"av_textblock_section av-kr6lu3mv-2ba78ab38de2a16ee1e70ec12be8308e \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><table class=\"table table-striped\" border=\"1\" cellpadding=\"2\">\n<tbody>\n<tr>\n<td>2010 global anthropogenic CO<sub>2<\/sub>&nbsp;multiplier (ACM)**<\/td>\n<td>&nbsp; 135<\/td>\n<\/tr>\n<tr>\n<td>1950 ACM<\/td>\n<td>&nbsp; &nbsp;38<\/td>\n<\/tr>\n<tr>\n<td>1900 ACM<\/td>\n<td>&nbsp; &nbsp;18<\/td>\n<\/tr>\n<tr>\n<td>Number of days for anthropogenic CO<sub>2<\/sub>&nbsp;to equal a year&rsquo;s worth of global volcanism<\/td>\n<td>&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;2.7<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<\/div><\/section><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-wtizsr-0ca3a9cb7616006d20d8333294026a5d\">\n#top .hr.hr-invisible.av-wtizsr-0ca3a9cb7616006d20d8333294026a5d{\nheight:30px;\n}\n<\/style>\n<div class=\"hr av-wtizsr-0ca3a9cb7616006d20d8333294026a5d hr-invisible  avia-builder-el-33  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-kr6lv3hy-6fd383d6cbdc7042e5cb349f1f6d7c86 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p>* Equivale al 2% de la capacidad mundial de generaci&oacute;n de electricidad con carb&oacute;n.<br>\n**Relaci&oacute;n entre el CO<sub>2<\/sub> antropog&eacute;nico anual (aproximadamente 35 Gt) y la estimaci&oacute;n m&aacute;xima preferida para el CO<sub>2<\/sub> <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;VOLC&Aacute;NICO&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;Cuerpo de roca que se compone de fragmentos de rocas o minerales derivados volc&aacute;nicamente que luego fueron transportados a cierta distancia de su lugar de origen.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/volcanico-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">volc&aacute;nico<\/a> anual.<br>\n<sup>+<\/sup>Datos de 2015 de <a href=\"https:\/\/www.iea.org\/publications\/freepublications\/publication\/co2-emissions-from-fuel-combustion-highlights-2017.html\">Emisiones de CO<sub>2<\/sub> de la combusti&oacute;n de combustibles de la AIE<\/a> edici&oacute;n de 2017.<\/p>\n<\/div><\/section><\/div>\n<\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>We prevent volcanic risks, through projects in different areas: Science, education and geo-conservation. There is no Natural Disasters. They are natural risks or hazards that impact vulnerable societies and become disasters through human mismanagement.<\/p>\n","protected":false},"author":8,"featured_media":10113,"parent":12581,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-12743","page","type-page","status-publish","has-post-thumbnail","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/pages\/12743","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=12743"}],"version-history":[{"count":0,"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/pages\/12743\/revisions"}],"up":[{"embeddable":true,"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/pages\/12581"}],"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=12743"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}