{"id":11776,"date":"2021-07-14T12:44:15","date_gmt":"2021-07-14T10:44:15","guid":{"rendered":"http:\/\/volcanx.cluster031.hosting.ovh.net\/?page_id=11776"},"modified":"2021-10-04T18:34:36","modified_gmt":"2021-10-04T16:34:36","slug":"deteccion-de-lahares","status":"publish","type":"page","link":"https:\/\/volcanofoundation.org\/es\/creando-conocimiento-de-los-riesgos\/monitorizacion\/hidrologia\/deteccion-de-lahares\/","title":{"rendered":"LAHAR"},"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-11776\"><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-11776\"><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-11776\"><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>La peligrosidad de los lahares<\/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  \"><p><section class=\"av_textblock_section av-kqt9tgn4-955ae44a3b12f5f76d41e08b4c147261 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p>Los cient&iacute;ficos que vigilan los volcanes se enfrentan al reto cr&iacute;tico de detectar un <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAHAR&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Tambi&eacute;n se llama flujo de lodo volc&aacute;nico o flujo de escombros. Una mezcla de agua y escombros volc&aacute;nicos que se mueve r&aacute;pidamente r&iacute;o abajo. La consistencia puede variar desde la del agua de plato fangosa hasta la del cemento h&uacute;medo, dependiendo de la relaci&oacute;n entre el agua y los escombros. Se forman de diversas maneras, principalmente por el r&aacute;pido derretimiento de la nieve y el hielo por los flujos pirocl&aacute;sticos, las intensas lluvias en dep&oacute;sitos de rocas volc&aacute;nicas sueltas, la ruptura de un lago represado por dep&oacute;sitos volc&aacute;nicos y como consecuencia de avalanchas de escombros.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/lahar-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lahar<\/a>. El <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAHAR&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Tambi&eacute;n se llama flujo de lodo volc&aacute;nico o flujo de escombros. Una mezcla de agua y escombros volc&aacute;nicos que se mueve r&aacute;pidamente r&iacute;o abajo. La consistencia puede variar desde la del agua de plato fangosa hasta la del cemento h&uacute;medo, dependiendo de la relaci&oacute;n entre el agua y los escombros. Se forman de diversas maneras, principalmente por el r&aacute;pido derretimiento de la nieve y el hielo por los flujos pirocl&aacute;sticos, las intensas lluvias en dep&oacute;sitos de rocas volc&aacute;nicas sueltas, la ruptura de un lago represado por dep&oacute;sitos volc&aacute;nicos y como consecuencia de avalanchas de escombros.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/lahar-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lahar<\/a> es una avalancha de sedimentos volc&aacute;nicos que deval&uacute;a todo lo que se encuentra a su paso. vigilar la llegada y el paso de flujos de escombros e inundaciones en los valles fluviales que drenan volcanes activos.<\/p>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-167ir7j-fe6c491c8b1310bcd62e2a2cf7bea254\">\n#top .hr.hr-invisible.av-167ir7j-fe6c491c8b1310bcd62e2a2cf7bea254{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-167ir7j-fe6c491c8b1310bcd62e2a2cf7bea254 hr-invisible  avia-builder-el-13  avia-builder-el-no-sibling \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n<p><strong>Los lahares pueden producirse debido a<\/strong>:<\/p>\n<p>1-Per&iacute;odos de <strong>lluvia intensa<\/strong>, no necesariamente coincidentes con per&iacute;odos de actividad volc&aacute;nica. Como ocurri&oacute; tras la erupci&oacute;n del volc&aacute;n Pinatubo en la isla de Luz&oacute;n, Filipinas, en 1991.<br>\n2-<strong>Fusi&oacute;n de glaciares<\/strong> en las partes altas de un volc&aacute;n durante la actividad volc&aacute;nica. Lo que ocurri&oacute; en el volc&aacute;n Nevado del Ru&iacute;z, Colombia, en 1985;<br>\n3-<strong>Vac&iacute;o de un lago<\/strong> alojado en la cima de un volc&aacute;n. Aumento del riesgo en el Pinatubo.<br>\n4-<strong>Colapso de la ladera<\/strong> debido a una perturbaci&oacute;n hidrot&eacute;rmica prolongada o a un terremoto. Como en el caso de la isla caribe&ntilde;a de Monserrat.<br>\nA diferencia de las avalanchas de escombros, los lahares son dep&oacute;sitos h&uacute;medos donde el agua influye tanto en la g&eacute;nesis como en el transporte de la masa removida.<\/p>\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-14  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-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-15  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-681ba37c5058455b6f8e29e7c8fc34ea\">\n.avia-image-container.av-kqtcpnnn-681ba37c5058455b6f8e29e7c8fc34ea img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-kqtcpnnn-681ba37c5058455b6f8e29e7c8fc34ea .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<\/p><div class=\"avia-image-container av-kqtcpnnn-681ba37c5058455b6f8e29e7c8fc34ea av-styling- avia-align-center  avia-builder-el-16  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-11782 avia-img-lazy-loading-not-11782 avia_image \" src=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/scientists-acoustic-flow-monistor.jpg\" alt=\"\" title=\"scientists-acoustic-flow-monistor\" height=\"769\" width=\"1140\" itemprop=\"thumbnailUrl\" srcset=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/scientists-acoustic-flow-monistor.jpg 1140w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/scientists-acoustic-flow-monistor-300x202.jpg 300w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/scientists-acoustic-flow-monistor-1030x695.jpg 1030w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/scientists-acoustic-flow-monistor-768x518.jpg 768w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/scientists-acoustic-flow-monistor-705x476.jpg 705w\" 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>Los cient&iacute;ficos mantienen un monitor de flujo ac&uacute;stico (AMF) en el Monte Santa Helena, Washington. Detecta el movimiento del suelo asociado a los lahares.<\/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-18  el_after_av_textblock  el_before_av_image \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-kqtq6km7-f224551fa73f554740d73319bdd94131\">\n.avia-image-container.av-kqtq6km7-f224551fa73f554740d73319bdd94131 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-kqtq6km7-f224551fa73f554740d73319bdd94131 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div class=\"avia-image-container av-kqtq6km7-f224551fa73f554740d73319bdd94131 av-styling- avia-align-center  avia-builder-el-19  el_after_av_hr  el_before_av_textblock \" 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-11785 avia-img-lazy-loading-not-11785 avia_image \" src=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/acoustic-flow-monitor-signal.jpg\" alt=\"\" title=\"acoustic-flow-monitor-signal\" height=\"498\" width=\"600\" itemprop=\"thumbnailUrl\" srcset=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/acoustic-flow-monitor-signal.jpg 600w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/acoustic-flow-monitor-signal-300x249.jpg 300w\" sizes=\"(max-width: 600px) 100vw, 600px\"\/><\/div><\/div><\/div><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-kqtq6xrn-48627c4a9ffbba4a53951da875f446da\">\n#top .av_textblock_section.av-kqtq6xrn-48627c4a9ffbba4a53951da875f446da .avia_textblock{\nfont-size:14px;\n}\n<\/style>\n<section class=\"av_textblock_section av-kqtq6xrn-48627c4a9ffbba4a53951da875f446da \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p><em>Ejemplo de se&ntilde;al del monitor de flujo ac&uacute;stico de un peque&ntilde;o <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAHAR&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Tambi&eacute;n se llama flujo de lodo volc&aacute;nico o flujo de escombros. Una mezcla de agua y escombros volc&aacute;nicos que se mueve r&aacute;pidamente r&iacute;o abajo. La consistencia puede variar desde la del agua de plato fangosa hasta la del cemento h&uacute;medo, dependiendo de la relaci&oacute;n entre el agua y los escombros. Se forman de diversas maneras, principalmente por el r&aacute;pido derretimiento de la nieve y el hielo por los flujos pirocl&aacute;sticos, las intensas lluvias en dep&oacute;sitos de rocas volc&aacute;nicas sueltas, la ruptura de un lago represado por dep&oacute;sitos volc&aacute;nicos y como consecuencia de avalanchas de escombros.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/lahar-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lahar<\/a> en la madrugada del 6 de octubre de 2004. Las vigencias en el suelo (eje y) aumentan a medida que el <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAHAR&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Tambi&eacute;n se llama flujo de lodo volc&aacute;nico o flujo de escombros. Una mezcla de agua y escombros volc&aacute;nicos que se mueve r&aacute;pidamente r&iacute;o abajo. La consistencia puede variar desde la del agua de plato fangosa hasta la del cemento h&uacute;medo, dependiendo de la relaci&oacute;n entre el agua y los escombros. Se forman de diversas maneras, principalmente por el r&aacute;pido derretimiento de la nieve y el hielo por los flujos pirocl&aacute;sticos, las intensas lluvias en dep&oacute;sitos de rocas volc&aacute;nicas sueltas, la ruptura de un lago represado por dep&oacute;sitos volc&aacute;nicos y como consecuencia de avalanchas de escombros.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/lahar-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lahar<\/a> pasa por la estaci&oacute;n.<\/em><\/p>\n<\/div><\/section><\/div>\n<\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Scientists who monitor volcanoes face the critical challenge of detecting a <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAHAR&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Tambi&eacute;n se llama flujo de lodo volc&aacute;nico o flujo de escombros. Una mezcla de agua y escombros volc&aacute;nicos que se mueve r&aacute;pidamente r&iacute;o abajo. La consistencia puede variar desde la del agua de plato fangosa hasta la del cemento h&uacute;medo, dependiendo de la relaci&oacute;n entre el agua y los escombros. Se forman de diversas maneras, principalmente por el r&aacute;pido derretimiento de la nieve y el hielo por los flujos pirocl&aacute;sticos, las intensas lluvias en dep&oacute;sitos de rocas volc&aacute;nicas sueltas, la ruptura de un lago represado por dep&oacute;sitos volc&aacute;nicos y como consecuencia de avalanchas de escombros.&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/lahar-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">lahar<\/a>. An avalanche and volcanic sediment flow that devalues everything in its path and creates unstoppable disasters.<\/p>\n","protected":false},"author":8,"featured_media":10113,"parent":11719,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-11776","page","type-page","status-publish","has-post-thumbnail","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/pages\/11776","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=11776"}],"version-history":[{"count":0,"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/pages\/11776\/revisions"}],"up":[{"embeddable":true,"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/pages\/11719"}],"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=11776"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}