{"id":11791,"date":"2021-07-14T12:43:59","date_gmt":"2021-07-14T10:43:59","guid":{"rendered":"http:\/\/volcanx.cluster031.hosting.ovh.net\/?page_id=11791"},"modified":"2021-10-04T18:29:22","modified_gmt":"2021-10-04T16:29:22","slug":"calor-termia","status":"publish","type":"page","link":"https:\/\/volcanofoundation.org\/es\/creando-conocimiento-de-los-riesgos\/monitorizacion\/calor-termia\/","title":{"rendered":"CALOR\/TERMIA"},"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-11791\"><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-11791\"><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-11791\"><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>Las temperaturas de la superficie reflejan las temperaturas del subsuelo<\/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>Algunos volcanes tienen caracter&iacute;sticas t&eacute;rmicas particulares<\/h3>\n<p>Algunos volcanes tienen caracter&iacute;sticas t&eacute;rmicas como respiraderos humeantes, g&eacute;iseres, fuentes termales, 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> 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>. El 60% de los volcanes activos carecen de un sistema de vigilancia de la superficie <a title=\"60% of ACTIVE VOLCANOES HAVE NO MONITORING SYSTEM\" href=\"http:\/\/volcanx.cluster031.hosting.ovh.net\/es\/el-60-de-los-volcanes-activos-no-tienen-sistema-de-vigilancia\/\">cambio de temperatura<\/a> en estas caracter&iacute;sticas t&eacute;rmicas a veces se produce antes de una erupci&oacute;n volc&aacute;nica. El reconocimiento de estas &laquo;anomal&iacute;as t&eacute;rmicas&raquo; puede ser &uacute;til para predecir <a title=\"MONITORING\" href=\"http:\/\/volcanx.cluster031.hosting.ovh.net\/es\/creando-conocimiento-de-los-riesgos\/monitoring\/\">cambios de actividad<\/a>.<\/p>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-71sbkoe-4fe8b15c7b594a2c6b2646153bbd3d97\">\n#top .hr.hr-invisible.av-71sbkoe-4fe8b15c7b594a2c6b2646153bbd3d97{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-71sbkoe-4fe8b15c7b594a2c6b2646153bbd3d97 hr-invisible  avia-builder-el-13  el_before_av_hr  avia-builder-el-first \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n<p><strong>Varias caracter&iacute;sticas t&eacute;rmicas son dignas de menci&oacute;n<\/strong><\/p>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-6mtia7i-e55b3575cdac2060be6996a46d30d1ef\">\n#top .hr.hr-invisible.av-6mtia7i-e55b3575cdac2060be6996a46d30d1ef{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-6mtia7i-e55b3575cdac2060be6996a46d30d1ef hr-invisible  avia-builder-el-14  el_after_av_hr  el_before_av_hr \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n<ol>\n<li><strong>Vapor<\/strong>, o rasgos dominados por el vapor, como respiraderos de gas, fumarolas y ollas de barro, var&iacute;an en temperatura desde la ebullici&oacute;n hasta varios cientos de grados (unos 400 &deg;C o 750 &deg;F).<\/li>\n<li>Los rasgos dominados por el agua incluyen g&eacute;iseres, manantiales\/piscinas calientes, lagos de cr&aacute;ter, temperatura elevada de la superficie del mar (por ejemplo, por la actividad volc&aacute;nica submarina o insular), e incluso el derretimiento del hielo (por ejemplo, volcanes subglaciales). La temperatura de estos fen&oacute;menos oscila entre la congelaci&oacute;n y la ebullici&oacute;n.<\/li>\n<li><strong>Las caracter&iacute;sticas dominadas por la <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><\/strong> incluyen lagos 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>, 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>, c&uacute;pulas 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> y flujos pirocl&aacute;sticos, y pueden alcanzar temperaturas de hasta unos 1200 &deg;C (2200 &deg;F).<\/li>\n<\/ol>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-6ad2lda-6b86ecf7102cc9559d4d4cc3ead599d9\">\n#top .hr.hr-invisible.av-6ad2lda-6b86ecf7102cc9559d4d4cc3ead599d9{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-6ad2lda-6b86ecf7102cc9559d4d4cc3ead599d9 hr-invisible  avia-builder-el-15  el_after_av_hr  avia-builder-el-last \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div>\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<div class=\"hr av-kqta1i5b-107d1a9c40127944f7fe3b907c4f1f41 hr-invisible  avia-builder-el-16  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-17  el_after_av_three_fifth  el_before_av_one_full  flex_column_div av-zero-column-padding  \"><p>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-kqtcpnnn-3d1f342d6f8b7b890d4895bc919dd362\">\n.avia-image-container.av-kqtcpnnn-3d1f342d6f8b7b890d4895bc919dd362 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-kqtcpnnn-3d1f342d6f8b7b890d4895bc919dd362 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<\/p><div class=\"avia-image-container av-kqtcpnnn-3d1f342d6f8b7b890d4895bc919dd362 av-styling- avia-align-center  avia-builder-el-18  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-11811 avia-img-lazy-loading-not-11811 avia_image \" src=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/scientist-temperatures-measurement.jpg\" alt=\"\" title=\"scientist-temperatures-measurement\" height=\"800\" width=\"500\" itemprop=\"thumbnailUrl\" srcset=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/scientist-temperatures-measurement.jpg 500w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/scientist-temperatures-measurement-188x300.jpg 188w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/scientist-temperatures-measurement-441x705.jpg 441w\" sizes=\"(max-width: 500px) 100vw, 500px\"\/><\/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>Norris-2003. un cient&iacute;fico de la YVO realiza una medici&oacute;n de temperatura en el &laquo;Hijo del Drag&oacute;n Verde&raquo; <span class=\"glossary-term\" title=\" data-original-title=\">caracter&iacute;stica <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;T&Eacute;RMICA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;De o relacionado con el calor. En los volcanes, se observan caracter&iacute;sticas t&eacute;rmicas para determinar si las temperaturas est&aacute;n cambiando (por ejemplo, fumarolas, respiraderos, superficies de lava, etc.). Estos cambios ayudan a los cient&iacute;ficos a entender los procesos volc&aacute;nicos.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/termica-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">t&eacute;rmica<\/a><\/span>.<\/em><\/p>\n<\/div><\/section>\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-20  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-mv8b8u-e8feeddcdacb26803d02d28473d3d58a\">\n.flex_column.av-mv8b8u-e8feeddcdacb26803d02d28473d3d58a{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-mv8b8u-e8feeddcdacb26803d02d28473d3d58a av_one_full  avia-builder-el-21  el_after_av_two_fifth  el_before_av_three_fifth  first flex_column_div av-zero-column-padding  \"><section class=\"av_textblock_section av-kqtrkuws-7b3419428b7f09a76d9849a905eca919 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p>Los rasgos t&eacute;rmicos dominados por el vapor y el agua se forman a medida que el <span class=\"glossary-term\" title=\" data-original-title=\"><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><\/span> bajo la superficie calienta las rocas y el agua subterr&aacute;nea que se encuentran sobre ella, lo que hace que los fluidos calentados circulen por convecci&oacute;n en las rocas suprayacentes.<\/p>\n<\/div><\/section><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-5qmflpq-289c3c39428682440e1f78a14e5dd324\">\n.flex_column.av-5qmflpq-289c3c39428682440e1f78a14e5dd324{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-5qmflpq-289c3c39428682440e1f78a14e5dd324 av_three_fifth  avia-builder-el-23  el_after_av_one_full  el_before_av_two_fifth  first flex_column_div av-zero-column-padding  column-top-margin\"><section class=\"av_textblock_section av-kqtqzo54-137a8364c2f7e4ac750aadc513a9eb82 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><h3>Las mediciones de la temperatura del suelo son importantes para el estudio completo de la evoluci&oacute;n de un volc&aacute;n<\/h3>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-5at2rwu-cd8a3bb9d2ea84d871934c8d9c36d26a\">\n#top .hr.hr-invisible.av-5at2rwu-cd8a3bb9d2ea84d871934c8d9c36d26a{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-5at2rwu-cd8a3bb9d2ea84d871934c8d9c36d26a 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>Medir directamente la temperatura de las cuencas de aguas termales, los campos de fumarolas o las corrientes 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> activas puede ser peligroso. Para realizar mediciones muy precisas, los cient&iacute;ficos colocan unos dispositivos llamados termopares directamente sobre la superficie caliente de un elemento t&eacute;rmico. Este tipo de mediciones se realizan con mayor frecuencia en volcanes de f&aacute;cil acceso, y los cient&iacute;ficos s&oacute;lo realizan las mediciones si las zonas son seguras durante varios minutos. Aunque las mediciones directas son muy precisas, son limitadas porque s&oacute;lo pueden cubrir un &aacute;rea peque&ntilde;a o espec&iacute;fica.<\/p>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-4n7as6m-1b69854abf63ee8958bf36e317b8ff6c\">\n#top .hr.hr-invisible.av-4n7as6m-1b69854abf63ee8958bf36e317b8ff6c{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-4n7as6m-1b69854abf63ee8958bf36e317b8ff6c 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>Las mediciones de temperatura tambi&eacute;n pueden realizarse a distancia mediante c&aacute;maras o instrumentos que miden la radiaci&oacute;n infrarroja <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;T&Eacute;RMICA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;De o relacionado con el calor. En los volcanes, se observan caracter&iacute;sticas t&eacute;rmicas para determinar si las temperaturas est&aacute;n cambiando (por ejemplo, fumarolas, respiraderos, superficies de lava, etc.). Estos cambios ayudan a los cient&iacute;ficos a entender los procesos volc&aacute;nicos.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/termica-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">t&eacute;rmica<\/a>, que se emite desde la superficie calentada. Sin embargo, la radiaci&oacute;n TIR puede quedar parcial o totalmente oculta por nubes espesas o penachos 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>, por lo que este tipo de mediciones deben realizarse en condiciones atmosf&eacute;ricas favorables. Un instrumento com&uacute;n utilizado por los cient&iacute;ficos del Programa de Riesgos Volc&aacute;nicos es una c&aacute;mara infrarroja (<a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;T&Eacute;RMICA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;De o relacionado con el calor. En los volcanes, se observan caracter&iacute;sticas t&eacute;rmicas para determinar si las temperaturas est&aacute;n cambiando (por ejemplo, fumarolas, respiraderos, superficies de lava, etc.). Estos cambios ayudan a los cient&iacute;ficos a entender los procesos volc&aacute;nicos.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/termica-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">t&eacute;rmica<\/a>) frontal, que produce una imagen utilizando un espectro de colores que se correlaciona con la temperatura detectada.<\/p>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-4jonvta-e20765737d3cc13887e83cbbe1065784\">\n#top .hr.hr-invisible.av-4jonvta-e20765737d3cc13887e83cbbe1065784{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-4jonvta-e20765737d3cc13887e83cbbe1065784 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<\/div><\/section><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-39k1nbi-955ccf39f1329f46b6bb95a7ab1193e4\">\n#top .hr.hr-invisible.av-39k1nbi-955ccf39f1329f46b6bb95a7ab1193e4{\nheight:30px;\n}\n<\/style>\n<div class=\"hr av-39k1nbi-955ccf39f1329f46b6bb95a7ab1193e4 hr-invisible  avia-builder-el-28  el_after_av_textblock  el_before_av_textblock \"><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-kqtr9nuf-1ad91b512b7cb99e299a9aa346839e40\">\n#top .av_textblock_section.av-kqtr9nuf-1ad91b512b7cb99e299a9aa346839e40 .avia_textblock{\nfont-size:14px;\n}\n<\/style>\n<section class=\"av_textblock_section av-kqtr9nuf-1ad91b512b7cb99e299a9aa346839e40 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p style=\"text-align: right;\"><em>Esta imagen muestra a un ge&oacute;logo de la HVO tomando muestras de la <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> que se filtraba del interior del escudo sin ra&iacute;ces. La <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> fue colocada en un cubo de agua para enfriar la muestra. El fotograma superior es una fotograf&iacute;a normal, mientras que el inferior es una imagen <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;T&Eacute;RMICA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;De o relacionado con el calor. En los volcanes, se observan caracter&iacute;sticas t&eacute;rmicas para determinar si las temperaturas est&aacute;n cambiando (por ejemplo, fumarolas, respiraderos, superficies de lava, etc.). Estos cambios ayudan a los cient&iacute;ficos a entender los procesos volc&aacute;nicos.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/termica-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">t&eacute;rmica<\/a> tomada a una fracci&oacute;n de segundo de la fotograf&iacute;a. Como muestra la imagen <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;T&Eacute;RMICA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;De o relacionado con el calor. En los volcanes, se observan caracter&iacute;sticas t&eacute;rmicas para determinar si las temperaturas est&aacute;n cambiando (por ejemplo, fumarolas, respiraderos, superficies de lava, etc.). Estos cambios ayudan a los cient&iacute;ficos a entender los procesos volc&aacute;nicos.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/termica-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">t&eacute;rmica<\/a>, el interior incandescente del flujo, que queda expuesto al desprenderse el clinker 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>, supera los 1000 grados Celsius (1800 grados Fahrenheit). El ge&oacute;logo se protege la cara del calor radiante.<\/em><\/p>\n<\/div><\/section><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-2trvoq6-c5814f587a08533aab8205f385a0be50\">\n.flex_column.av-2trvoq6-c5814f587a08533aab8205f385a0be50{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-2trvoq6-c5814f587a08533aab8205f385a0be50 av_two_fifth  avia-builder-el-30  el_after_av_three_fifth  el_before_av_three_fifth  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-kqtq6km7-f3523afe1982cf570688c38a6b74603c\">\n.avia-image-container.av-kqtq6km7-f3523afe1982cf570688c38a6b74603c img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-kqtq6km7-f3523afe1982cf570688c38a6b74603c .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<\/p><div class=\"avia-image-container av-kqtq6km7-f3523afe1982cf570688c38a6b74603c av-styling- avia-align-center  avia-builder-el-31  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-11814 avia-img-lazy-loading-not-11814 avia_image \" src=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/thermocouple-temperature-measurement.jpg\" alt=\"\" title=\"thermocouple-temperature-measurement\" height=\"760\" width=\"1140\" itemprop=\"thumbnailUrl\" srcset=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/thermocouple-temperature-measurement.jpg 1140w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/thermocouple-temperature-measurement-300x200.jpg 300w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/thermocouple-temperature-measurement-1030x687.jpg 1030w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/thermocouple-temperature-measurement-768x512.jpg 768w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/thermocouple-temperature-measurement-705x470.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-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>Medici&oacute;n de la temperatura de un termopar en el <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;FLUJO DE LAVA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Los flujos de lava son masas de roca fundida que se vierten sobre la superficie de la Tierra durante una erupci&oacute;n efusiva. Tanto la lava m&oacute;vil como el dep&oacute;sito solidificado resultante se conocen como flujos de lava. Debido a la amplia gama en viscosidad de los diferentes tipos de lava (basalto, andesita, dacita y riolita); descarga de lava durante las erupciones; y caracter&iacute;sticas del respiradero en erupci&oacute;n y la topograf&iacute;a sobre la que viaja la lava, los flujos de lava vienen en una gran variedad de formas y tama&ntilde;os.&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/flujo-lava-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">flujo de lava<\/a> del 27 de junio, volc&aacute;n K&#299;lauea, Hawai. Temperatura calculada de 1100&ordm;C (2012&ordm;F) a 3 km de la fuente de Pu&rsquo;u &lsquo;&#332;&rsquo;&#333;.<\/em><\/p>\n<\/div><\/section>\n<p>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-2e2igoe-9119e9a646b57209b89efa73fb3b9eb6\">\n#top .hr.hr-invisible.av-2e2igoe-9119e9a646b57209b89efa73fb3b9eb6{\nheight:30px;\n}\n<\/style>\n<\/p><div class=\"hr av-2e2igoe-9119e9a646b57209b89efa73fb3b9eb6 hr-invisible  avia-builder-el-33  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-kqtr9bos-77b5dd8ddcb32ada54a237c2adea8c4c\">\n.avia-image-container.av-kqtr9bos-77b5dd8ddcb32ada54a237c2adea8c4c img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-kqtr9bos-77b5dd8ddcb32ada54a237c2adea8c4c .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div class=\"avia-image-container av-kqtr9bos-77b5dd8ddcb32ada54a237c2adea8c4c av-styling- avia-align-center  avia-builder-el-34  el_after_av_hr  el_before_av_hr \" 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-11817 avia-img-lazy-loading-not-11817 avia_image \" src=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/photo-compared-thermal-image.jpg\" alt=\"\" title=\"photo-compared-thermal-image\" height=\"1200\" width=\"898\" itemprop=\"thumbnailUrl\" srcset=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/photo-compared-thermal-image.jpg 898w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/photo-compared-thermal-image-225x300.jpg 225w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/photo-compared-thermal-image-771x1030.jpg 771w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/photo-compared-thermal-image-768x1026.jpg 768w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/photo-compared-thermal-image-528x705.jpg 528w\" sizes=\"(max-width: 898px) 100vw, 898px\"\/><\/div><\/div><\/div><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-1jik4jy-ad5a2aa6b839ef2898ac6cf7d56cffa7\">\n#top .hr.hr-invisible.av-1jik4jy-ad5a2aa6b839ef2898ac6cf7d56cffa7{\nheight:30px;\n}\n<\/style>\n<div class=\"hr av-1jik4jy-ad5a2aa6b839ef2898ac6cf7d56cffa7 hr-invisible  avia-builder-el-35  el_after_av_image  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-1i053v2-905c43c64eb4da94a62d13d12964ebaa\">\n.flex_column.av-1i053v2-905c43c64eb4da94a62d13d12964ebaa{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-1i053v2-905c43c64eb4da94a62d13d12964ebaa av_three_fifth  avia-builder-el-36  el_after_av_two_fifth  el_before_av_two_fifth  first flex_column_div av-zero-column-padding  \"><section class=\"av_textblock_section av-kqtrgmh5-1e9d4117dfa65a4d8877390b78af7c1a \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><h3>Los sat&eacute;lites pueden detectar las caracter&iacute;sticas t&eacute;rmicas de los volcanes<\/h3>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-14bj1xq-b007476c4e9eeea278179b127566fe3f\">\n#top .hr.hr-invisible.av-14bj1xq-b007476c4e9eeea278179b127566fe3f{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-14bj1xq-b007476c4e9eeea278179b127566fe3f hr-invisible  avia-builder-el-38  avia-builder-el-no-sibling \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n<p>Se trata de una herramienta importante para vigilar volcanes remotos con pocas instalaciones en tierra. Algunos sensores satelitales realizan observaciones diarias o semidiarias sobre los volcanes, pero estos sensores registran im&aacute;genes de grandes &aacute;reas con baja resoluci&oacute;n, lo que limita el detalle a peque&ntilde;a escala que puede verse de las caracter&iacute;sticas t&eacute;rmicas. Se pueden obtener im&aacute;genes TIR m&aacute;s detalladas y de mayor resoluci&oacute;n a partir de sensores satelitales y a&eacute;reos, pero las observaciones suelen ser menos frecuentes.<\/p>\n<\/div><\/section><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-ngd77y-6b60d2f6d92e861b0ec3aafca7b4e84f\">\n#top .hr.hr-invisible.av-ngd77y-6b60d2f6d92e861b0ec3aafca7b4e84f{\nheight:30px;\n}\n<\/style>\n<div class=\"hr av-ngd77y-6b60d2f6d92e861b0ec3aafca7b4e84f hr-invisible  avia-builder-el-39  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-27op566-b6c5f6e64615d7d763f43a2d8138ec0d\">\n.flex_column.av-27op566-b6c5f6e64615d7d763f43a2d8138ec0d{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-27op566-b6c5f6e64615d7d763f43a2d8138ec0d av_two_fifth  avia-builder-el-40  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-kqtrbd6a-8b74622fbea3acbce2c47faca05c1b72\">\n.avia-image-container.av-kqtrbd6a-8b74622fbea3acbce2c47faca05c1b72 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-kqtrbd6a-8b74622fbea3acbce2c47faca05c1b72 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<\/p><div class=\"avia-image-container av-kqtrbd6a-8b74622fbea3acbce2c47faca05c1b72 av-styling- avia-align-center  avia-builder-el-41  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-11820 avia-img-lazy-loading-not-11820 avia_image \" src=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/composite-satellite-image.jpg\" alt=\"\" title=\"composite-satellite-image\" height=\"554\" width=\"800\" itemprop=\"thumbnailUrl\" srcset=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/composite-satellite-image.jpg 800w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/composite-satellite-image-300x208.jpg 300w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/composite-satellite-image-768x532.jpg 768w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/composite-satellite-image-705x488.jpg 705w\" sizes=\"(max-width: 800px) 100vw, 800px\"\/><\/div><\/div><\/div><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-kqtrbmk5-8ac24eba9a05677c33f4fec27dc5b372\">\n#top .av_textblock_section.av-kqtrbmk5-8ac24eba9a05677c33f4fec27dc5b372 .avia_textblock{\nfont-size:14px;\n}\n<\/style>\n<section class=\"av_textblock_section av-kqtrbmk5-8ac24eba9a05677c33f4fec27dc5b372 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p><em>Imagen satelital compuesta del volc&aacute;n Veniaminof (Alaska) recogida por Landsat-8 con datos infrarrojos de onda corta para mostrar 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> t&eacute;rmicas del <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;FLUJO DE LAVA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Los flujos de lava son masas de roca fundida que se vierten sobre la superficie de la Tierra durante una erupci&oacute;n efusiva. Tanto la lava m&oacute;vil como el dep&oacute;sito solidificado resultante se conocen como flujos de lava. Debido a la amplia gama en viscosidad de los diferentes tipos de lava (basalto, andesita, dacita y riolita); descarga de lava durante las erupciones; y caracter&iacute;sticas del respiradero en erupci&oacute;n y la topograf&iacute;a sobre la que viaja la lava, los flujos de lava vienen en una gran variedad de formas y tama&ntilde;os.&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/flujo-lava-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">flujo de lava<\/a> activo superpuestas a una imagen de longitud de onda visible. En junio de 2013 comenz&oacute; una erupci&oacute;n con efusi&oacute;n 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> y <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> <span class=\"glossary-term\" title=\" data-original-title=\">emisi&oacute;n<\/span>, seguida de una pausa en la actividad. La corriente 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> activa se muestra en tonos amarillos y naranjas, y se extiende hacia el sur desde la chimenea. En la nieve y el hielo se observan finos dep&oacute;sitos 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> volc&aacute;nica, como radios radiales que se forman cuando 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> se emite bajo la direcci&oacute;n cambiante del viento.<\/em><\/p>\n<\/div><\/section><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-lfm13i-09b5af4c698dcd7a9ab3151cdebd10ac\">\n#top .hr.hr-invisible.av-lfm13i-09b5af4c698dcd7a9ab3151cdebd10ac{\nheight:30px;\n}\n<\/style>\n<div class=\"hr av-lfm13i-09b5af4c698dcd7a9ab3151cdebd10ac hr-invisible  avia-builder-el-43  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>Some volcanoes have particular thermal characteristics. These characteristics are important to know the state of the volcano and mitigating risks.<\/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-11791","page","type-page","status-publish","has-post-thumbnail","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/pages\/11791","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=11791"}],"version-history":[{"count":0,"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/pages\/11791\/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=11791"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}