{"id":11792,"date":"2021-07-14T12:47:02","date_gmt":"2021-07-14T10:47:02","guid":{"rendered":"http:\/\/volcanx.cluster031.hosting.ovh.net\/?page_id=11792"},"modified":"2021-07-15T12:03:49","modified_gmt":"2021-07-15T10:03:49","slug":"chaleur-thermal","status":"publish","type":"page","link":"https:\/\/volcanofoundation.org\/fr\/renforcer-la-connaissance-des-risques\/monitoring\/chaleur-thermal\/","title":{"rendered":"CHALEUR\/THERMAL"},"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-11792\"><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;\">RENFORCER LA CONNAISSANCE DES RISQUES<\/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;\">POURQUOI LA FONDATION EST N&Eacute;E ?<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-11792\"><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>LES DISASTERS NE SONT PAS NATURELS<\/strong><\/a>, ils sont construits socialement, par manque de pr&eacute;paration, de pr&eacute;vention, de travail d&rsquo;att&eacute;nuation, d&rsquo;&eacute;ducation et de suivi. <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;CE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Abr&eacute;viation de &amp;quot;l&amp;#039;&egrave;re commune&amp;quot; ou &amp;quot;l&amp;#039;&egrave;re actuelle&amp;quot;. CE se r&eacute;f&egrave;re &agrave; l&amp;#039;ann&eacute;e &eacute;coul&eacute;e depuis le d&eacute;but de l&amp;#039;&egrave;re actuelle dans le calendrier julien ou gr&eacute;gorien, par exemple l&amp;#039;ann&eacute;e civile. L&amp;#039;&egrave;re pr&eacute;c&eacute;dente est appel&eacute;e &amp;quot;Avant l&amp;#039;&egrave;re actuelle&amp;quot; ou BCE.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/ce-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>Ce<\/a> sont des risques ou des dangers naturels qui ont un impact sur les soci&eacute;t&eacute;s vuln&eacute;rables. Les connaissances aident &agrave; <strong>r&eacute;duire la vuln&eacute;rabilit&eacute; sociale<\/strong> et <strong>structurale<\/strong> afin d&rsquo;avoir des soci&eacute;t&eacute;s plus <strong>r&eacute;silientes<\/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-11792\"><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>Les temp&eacute;ratures de surface refl&egrave;tent les temp&eacute;ratures sous le sol<\/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>Certains volcans ont des caract&eacute;ristiques thermiques particuli&egrave;res<\/h3>\n<p>Certains volcans pr&eacute;sentent des caract&eacute;ristiques thermiques particuli&egrave;res telles que des &eacute;vents fumants, des geysers, des sources chaudes, des coul&eacute;es de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Terme g&eacute;n&eacute;ral d&eacute;signant le magma (roche en fusion) qui a fait &eacute;ruption &agrave; la surface de la Terre et qui conserve son int&eacute;grit&eacute; sous forme de masse fluide ou visqueuse, plut&ocirc;t que d&amp;#039;exploser en fragments.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/lave-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lave<\/a> ou des d&ocirc;mes de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Terme g&eacute;n&eacute;ral d&eacute;signant le magma (roche en fusion) qui a fait &eacute;ruption &agrave; la surface de la Terre et qui conserve son int&eacute;grit&eacute; sous forme de masse fluide ou visqueuse, plut&ocirc;t que d&amp;#039;exploser en fragments.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/lave-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lave<\/a>. Des changements de surface <a title=\"60% DES VOLCANS ACTIFS N'ONT PAS DE SYST&Egrave;ME DE SURVEILLANCE\" href=\"http:\/\/volcanx.cluster031.hosting.ovh.net\/es\/el-60-de-los-volcanes-activos-no-tienen-sistema-de-vigilancia\/\">temp&eacute;rature<\/a> au niveau de ces caract&eacute;ristiques thermiques se produisent parfois avant une &eacute;ruption volcanique. La reconnaissance de ces &laquo;&nbsp;anomalies thermiques&nbsp;&raquo; peut &ecirc;tre utile pour pr&eacute;dire <a title=\"MONITORING\" href=\"http:\/\/volcanx.cluster031.hosting.ovh.net\/es\/creando-conocimiento-de-los-riesgos\/monitoring\/\">les changements d&rsquo;activit&eacute;<\/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>Plusieurs caract&eacute;ristiques thermiques sont &agrave; noter<\/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>Les caract&eacute;ristiques domin&eacute;es par la vapeur<\/strong>, comme les &eacute;vents de gaz, les fumerolles et les marmites de boue, ont une temp&eacute;rature allant de l&rsquo;&eacute;bullition &agrave; plusieurs centaines de degr&eacute;s (environ 400 &deg;C ou 750 &deg;F).<\/li>\n<li><strong>Les caract&eacute;ristiques domin&eacute;es par l&rsquo;eau<\/strong> comprennent les geysers, les sources\/piscines chaudes, les lacs de crat&egrave;re, l&rsquo;&eacute;l&eacute;vation de la temp&eacute;rature de la surface de la mer (par exemple, &agrave; cause de l&rsquo;activit&eacute; volcanique sous-marine ou insulaire), et m&ecirc;me la fonte de la glace (par exemple, les volcans sous-glaciaires). Leur temp&eacute;rature varie du gel &agrave; l&rsquo;&eacute;bullition.<\/li>\n<li><strong>Les caract&eacute;ristiques domin&eacute;es par la <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Terme g&eacute;n&eacute;ral d&eacute;signant le magma (roche en fusion) qui a fait &eacute;ruption &agrave; la surface de la Terre et qui conserve son int&eacute;grit&eacute; sous forme de masse fluide ou visqueuse, plut&ocirc;t que d&amp;#039;exploser en fragments.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/lave-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lave<\/a><\/strong> comprennent les lacs de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Terme g&eacute;n&eacute;ral d&eacute;signant le magma (roche en fusion) qui a fait &eacute;ruption &agrave; la surface de la Terre et qui conserve son int&eacute;grit&eacute; sous forme de masse fluide ou visqueuse, plut&ocirc;t que d&amp;#039;exploser en fragments.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/lave-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lave<\/a>, les coul&eacute;es de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Terme g&eacute;n&eacute;ral d&eacute;signant le magma (roche en fusion) qui a fait &eacute;ruption &agrave; la surface de la Terre et qui conserve son int&eacute;grit&eacute; sous forme de masse fluide ou visqueuse, plut&ocirc;t que d&amp;#039;exploser en fragments.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/lave-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lave<\/a>, les d&ocirc;mes de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Terme g&eacute;n&eacute;ral d&eacute;signant le magma (roche en fusion) qui a fait &eacute;ruption &agrave; la surface de la Terre et qui conserve son int&eacute;grit&eacute; sous forme de masse fluide ou visqueuse, plut&ocirc;t que d&amp;#039;exploser en fragments.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/lave-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lave<\/a> et les coul&eacute;es pyroclastiques, et peuvent atteindre des temp&eacute;ratures allant jusqu&rsquo;&agrave; environ 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-9e429384307994d1ac8e14274eb29f0e\">\n.avia-image-container.av-kqtcpnnn-9e429384307994d1ac8e14274eb29f0e img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-kqtcpnnn-9e429384307994d1ac8e14274eb29f0e .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<\/p><div class=\"avia-image-container av-kqtcpnnn-9e429384307994d1ac8e14274eb29f0e 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-11810 avia-img-lazy-loading-not-11810 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 scientifique de l&rsquo;YVO prend une mesure de temp&eacute;rature au &laquo;&nbsp;Fils du dragon vert&nbsp;&raquo; <span class=\"glossary-term\" title=\"\" data-original-title=\"De ou relatif &agrave; la chaleur. Sur les volcans, les caract&eacute;ristiques thermiques sont observ&eacute;es pour d&eacute;terminer si les temp&eacute;ratures changent (par exemple les fumerolles, les &eacute;vents, les surfaces de lave, etc...). Ces changements aident les scientifiques &agrave; comprendre les processus volcaniques.\">caract&eacute;ristiques thermiques<\/span>.<\/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-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>Les caract&eacute;ristiques thermiques domin&eacute;es par la vapeur et l&rsquo;eau se forment lorsque le <span class=\"glossary-term\" title=\"\" data-original-title=\"Roche fondue sous la surface de la Terre.\"><a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;MAGMA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Roche fondue sous la surface de la Terre.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/magma-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>magma<\/a><\/span> sous la surface chauffe les roches et les eaux souterraines au-dessus, <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;CE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Abr&eacute;viation de &amp;quot;l&amp;#039;&egrave;re commune&amp;quot; ou &amp;quot;l&amp;#039;&egrave;re actuelle&amp;quot;. CE se r&eacute;f&egrave;re &agrave; l&amp;#039;ann&eacute;e &eacute;coul&eacute;e depuis le d&eacute;but de l&amp;#039;&egrave;re actuelle dans le calendrier julien ou gr&eacute;gorien, par exemple l&amp;#039;ann&eacute;e civile. L&amp;#039;&egrave;re pr&eacute;c&eacute;dente est appel&eacute;e &amp;quot;Avant l&amp;#039;&egrave;re actuelle&amp;quot; ou BCE.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/ce-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>ce<\/a> qui fait circuler les fluides chauff&eacute;s par convection dans les roches sus-jacentes.<\/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>Les mesures de la temp&eacute;rature du sol sont importantes pour l&rsquo;&eacute;tude compl&egrave;te de l&rsquo;&eacute;volution d&rsquo;un volcan<\/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>Il peut &ecirc;tre dangereux de mesurer directement la temp&eacute;rature des bassins de sources chaudes, des champs de fumerolles ou des coul&eacute;es de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Terme g&eacute;n&eacute;ral d&eacute;signant le magma (roche en fusion) qui a fait &eacute;ruption &agrave; la surface de la Terre et qui conserve son int&eacute;grit&eacute; sous forme de masse fluide ou visqueuse, plut&ocirc;t que d&amp;#039;exploser en fragments.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/lave-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lave<\/a> actives. Pour des mesures tr&egrave;s pr&eacute;cises, les scientifiques placent des dispositifs appel&eacute;s thermocouples directement sur la surface chaude d&rsquo;un &eacute;l&eacute;ment <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;THERMIQUE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;En relation avec la chaleur. Aux volcans, des caract&eacute;ristiques thermiques sont observ&eacute;es pour d&eacute;terminer si les temp&eacute;ratures changent (par exemple fumaroles, &eacute;vents, surfaces de lave, etc.). Ces changements aident les scientifiques &agrave; comprendre les processus volcaniques.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/thermique-fr\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">thermique<\/a>. Ces mesures sont le plus souvent effectu&eacute;es sur des volcans facilement accessibles, et les scientifiques ne proc&egrave;dent aux mesures que si les zones sont s&ucirc;res pendant plusieurs minutes. Bien que les mesures directes soient tr&egrave;s pr&eacute;cises, elles sont limit&eacute;es car elles ne peuvent couvrir qu&rsquo;une zone petite ou sp&eacute;cifique.<\/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>Les mesures de temp&eacute;rature peuvent &eacute;galement &ecirc;tre effectu&eacute;es &agrave; distance &agrave; l&rsquo;aide de cam&eacute;ras ou d&rsquo;instruments qui mesurent le rayonnement infrarouge <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;THERMIQUE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;En relation avec la chaleur. Aux volcans, des caract&eacute;ristiques thermiques sont observ&eacute;es pour d&eacute;terminer si les temp&eacute;ratures changent (par exemple fumaroles, &eacute;vents, surfaces de lave, etc.). Ces changements aident les scientifiques &agrave; comprendre les processus volcaniques.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/thermique-fr\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">thermique<\/a>, qui est &eacute;mis par la surface chauff&eacute;e. Cependant, le rayonnement infrarouge <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;THERMIQUE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;En relation avec la chaleur. Aux volcans, des caract&eacute;ristiques thermiques sont observ&eacute;es pour d&eacute;terminer si les temp&eacute;ratures changent (par exemple fumaroles, &eacute;vents, surfaces de lave, etc.). Ces changements aident les scientifiques &agrave; comprendre les processus volcaniques.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/thermique-fr\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">thermique<\/a> peut &ecirc;tre partiellement ou totalement obscurci par d&rsquo;&eacute;pais nuages ou panaches de cendres, de sorte que ces types de mesures doivent &ecirc;tre effectu&eacute;s dans des conditions atmosph&eacute;riques favorables. Un instrument couramment utilis&eacute; par les scientifiques du programme sur les risques volcaniques est une cam&eacute;ra infrarouge (<a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;THERMIQUE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;En relation avec la chaleur. Aux volcans, des caract&eacute;ristiques thermiques sont observ&eacute;es pour d&eacute;terminer si les temp&eacute;ratures changent (par exemple fumaroles, &eacute;vents, surfaces de lave, etc.). Ces changements aident les scientifiques &agrave; comprendre les processus volcaniques.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/thermique-fr\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">thermique<\/a>) frontale, qui produit une image utilisant un spectre de couleurs en corr&eacute;lation avec la temp&eacute;rature d&eacute;tect&eacute;e.<\/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>Cette image montre un g&eacute;ologue du HVO en train de pr&eacute;lever un &eacute;chantillon de la <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Terme g&eacute;n&eacute;ral d&eacute;signant le magma (roche en fusion) qui a fait &eacute;ruption &agrave; la surface de la Terre et qui conserve son int&eacute;grit&eacute; sous forme de masse fluide ou visqueuse, plut&ocirc;t que d&amp;#039;exploser en fragments.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/lave-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lave<\/a> qui s&rsquo;infiltrait &agrave; l&rsquo;int&eacute;rieur du bouclier sans racines. La <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Terme g&eacute;n&eacute;ral d&eacute;signant le magma (roche en fusion) qui a fait &eacute;ruption &agrave; la surface de la Terre et qui conserve son int&eacute;grit&eacute; sous forme de masse fluide ou visqueuse, plut&ocirc;t que d&amp;#039;exploser en fragments.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/lave-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lave<\/a> a &eacute;t&eacute; plac&eacute;e dans un seau d&rsquo;eau pour tremper l&rsquo;&eacute;chantillon. Le cadre sup&eacute;rieur est une photographie normale, tandis que le cadre inf&eacute;rieur est une image <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;THERMIQUE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;En relation avec la chaleur. Aux volcans, des caract&eacute;ristiques thermiques sont observ&eacute;es pour d&eacute;terminer si les temp&eacute;ratures changent (par exemple fumaroles, &eacute;vents, surfaces de lave, etc.). Ces changements aident les scientifiques &agrave; comprendre les processus volcaniques.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/thermique-fr\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">thermique<\/a> prise &agrave; une fraction de seconde de la photographie. Comme le montre l&rsquo;image <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;THERMIQUE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;En relation avec la chaleur. Aux volcans, des caract&eacute;ristiques thermiques sont observ&eacute;es pour d&eacute;terminer si les temp&eacute;ratures changent (par exemple fumaroles, &eacute;vents, surfaces de lave, etc.). Ces changements aident les scientifiques &agrave; comprendre les processus volcaniques.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/thermique-fr\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">thermique<\/a>, l&rsquo;int&eacute;rieur incandescent de la <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;COUL&Eacute;E&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Un d&ocirc;me de lave allong&eacute; qui se forme g&eacute;n&eacute;ralement sous la forme d&amp;#039;une lave &agrave; haute silice &eacute;clate sur le flanc abrupt d&amp;#039;un volcan. L&amp;#039;axe du d&ocirc;me perpendiculaire &agrave; la pente du volcan est plus court que l&amp;#039;axe parall&egrave;le &agrave; la pente, cr&eacute;ant une forme elliptique. Le bord d&amp;#039;attaque de la coul&eacute;e est souvent bloc et escarp&eacute;.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/coulee-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>coul&eacute;e<\/a>, qui est expos&eacute; lorsque le clinker de la <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Terme g&eacute;n&eacute;ral d&eacute;signant le magma (roche en fusion) qui a fait &eacute;ruption &agrave; la surface de la Terre et qui conserve son int&eacute;grit&eacute; sous forme de masse fluide ou visqueuse, plut&ocirc;t que d&amp;#039;exploser en fragments.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/lave-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lave<\/a> se d&eacute;tache, d&eacute;passe 1000 degr&eacute;s Celsius (1800 degr&eacute;s Fahrenheit). Le g&eacute;ologue se prot&egrave;ge le visage de la chaleur rayonnante.<\/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-d0cdf226460b99f6f51d67c2ac32da10\">\n.avia-image-container.av-kqtq6km7-d0cdf226460b99f6f51d67c2ac32da10 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-kqtq6km7-d0cdf226460b99f6f51d67c2ac32da10 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<\/p><div class=\"avia-image-container av-kqtq6km7-d0cdf226460b99f6f51d67c2ac32da10 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-11813 avia-img-lazy-loading-not-11813 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>Mesure de la temp&eacute;rature par thermocouple d&rsquo;un d&eacute;bordement de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Terme g&eacute;n&eacute;ral d&eacute;signant le magma (roche en fusion) qui a fait &eacute;ruption &agrave; la surface de la Terre et qui conserve son int&eacute;grit&eacute; sous forme de masse fluide ou visqueuse, plut&ocirc;t que d&amp;#039;exploser en fragments.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/lave-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lave<\/a> de la <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;COUL&Eacute;E&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Un d&ocirc;me de lave allong&eacute; qui se forme g&eacute;n&eacute;ralement sous la forme d&amp;#039;une lave &agrave; haute silice &eacute;clate sur le flanc abrupt d&amp;#039;un volcan. L&amp;#039;axe du d&ocirc;me perpendiculaire &agrave; la pente du volcan est plus court que l&amp;#039;axe parall&egrave;le &agrave; la pente, cr&eacute;ant une forme elliptique. Le bord d&amp;#039;attaque de la coul&eacute;e est souvent bloc et escarp&eacute;.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/coulee-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>coul&eacute;e<\/a> de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Terme g&eacute;n&eacute;ral d&eacute;signant le magma (roche en fusion) qui a fait &eacute;ruption &agrave; la surface de la Terre et qui conserve son int&eacute;grit&eacute; sous forme de masse fluide ou visqueuse, plut&ocirc;t que d&amp;#039;exploser en fragments.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/lave-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lave<\/a> du 27 juin, volcan K&#299;lauea, Hawai&rsquo;i. Temp&eacute;rature globale calcul&eacute;e de 1100&ordm;C (2012&ordm;F) &agrave; 3 km (1,9 mi) de l&rsquo;<a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;&Eacute;VENT&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;Toute ouverture &agrave; la surface de la Terre par laquelle le magma entre en &eacute;ruption ou les gaz volcaniques sont &eacute;mis.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/event-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>&eacute;vent<\/a> source du Pu&rsquo;u &lsquo;&#332;&rsquo;&#333;.<\/em><\/p>\n<\/div><\/section><br>\n\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<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-86a0433735fe0a8658deb065453e7c74\">\n.avia-image-container.av-kqtr9bos-86a0433735fe0a8658deb065453e7c74 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-kqtr9bos-86a0433735fe0a8658deb065453e7c74 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div class=\"avia-image-container av-kqtr9bos-86a0433735fe0a8658deb065453e7c74 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-11816 avia-img-lazy-loading-not-11816 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>Les satellites peuvent d&eacute;tecter les caract&eacute;ristiques thermiques des volcans<\/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>Il s&rsquo;agit d&rsquo;un outil important pour la surveillance des volcans &eacute;loign&eacute;s disposant de peu d&rsquo;installations au sol. Certains capteurs satellitaires font des observations quotidiennes ou semi-quotidiennes au-dessus des volcans, mais ces capteurs enregistrent des images de grandes zones avec une faible r&eacute;solution, <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;CE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Abr&eacute;viation de &amp;quot;l&amp;#039;&egrave;re commune&amp;quot; ou &amp;quot;l&amp;#039;&egrave;re actuelle&amp;quot;. CE se r&eacute;f&egrave;re &agrave; l&amp;#039;ann&eacute;e &eacute;coul&eacute;e depuis le d&eacute;but de l&amp;#039;&egrave;re actuelle dans le calendrier julien ou gr&eacute;gorien, par exemple l&amp;#039;ann&eacute;e civile. L&amp;#039;&egrave;re pr&eacute;c&eacute;dente est appel&eacute;e &amp;quot;Avant l&amp;#039;&egrave;re actuelle&amp;quot; ou BCE.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/ce-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>ce<\/a> qui limite les d&eacute;tails &agrave; petite &eacute;chelle que l&rsquo;on peut voir des caract&eacute;ristiques thermiques. Des images TIR plus d&eacute;taill&eacute;es et &agrave; plus haute r&eacute;solution peuvent &ecirc;tre obtenues &agrave; partir de capteurs satellites et a&eacute;roport&eacute;s, mais les observations sont g&eacute;n&eacute;ralement moins fr&eacute;quentes.<\/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-01b07f2c3c1cd035fd8855e9360fb3b2\">\n.avia-image-container.av-kqtrbd6a-01b07f2c3c1cd035fd8855e9360fb3b2 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-kqtrbd6a-01b07f2c3c1cd035fd8855e9360fb3b2 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<\/p><div class=\"avia-image-container av-kqtrbd6a-01b07f2c3c1cd035fd8855e9360fb3b2 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-11819 avia-img-lazy-loading-not-11819 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>Image satellite composite du volcan Veniaminof (Alaska) collect&eacute;e par Landsat-8 avec des donn&eacute;es infrarouges &agrave; ondes courtes pour montrer les &eacute;missions thermiques de la <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;COUL&Eacute;E&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Un d&ocirc;me de lave allong&eacute; qui se forme g&eacute;n&eacute;ralement sous la forme d&amp;#039;une lave &agrave; haute silice &eacute;clate sur le flanc abrupt d&amp;#039;un volcan. L&amp;#039;axe du d&ocirc;me perpendiculaire &agrave; la pente du volcan est plus court que l&amp;#039;axe parall&egrave;le &agrave; la pente, cr&eacute;ant une forme elliptique. Le bord d&amp;#039;attaque de la coul&eacute;e est souvent bloc et escarp&eacute;.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/coulee-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>coul&eacute;e<\/a> de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Terme g&eacute;n&eacute;ral d&eacute;signant le magma (roche en fusion) qui a fait &eacute;ruption &agrave; la surface de la Terre et qui conserve son int&eacute;grit&eacute; sous forme de masse fluide ou visqueuse, plut&ocirc;t que d&amp;#039;exploser en fragments.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/lave-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lave<\/a> active superpos&eacute;es &agrave; une image &agrave; longueur d&rsquo;onde visible. Une &eacute;ruption a commenc&eacute; en juin 2013 avec des effusions de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Terme g&eacute;n&eacute;ral d&eacute;signant le magma (roche en fusion) qui a fait &eacute;ruption &agrave; la surface de la Terre et qui conserve son int&eacute;grit&eacute; sous forme de masse fluide ou visqueuse, plut&ocirc;t que d&amp;#039;exploser en fragments.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/lave-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lave<\/a> et des <span class=\"glossary-term\" title=\"\" data-original-title=\"La lib&eacute;ration de gaz volcaniques de la terre, qui s'&eacute;chappent dans l'atmosph&egrave;re.\">&eacute;missions<\/span>, suivie d&rsquo;une accalmie. La <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;COUL&Eacute;E&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Un d&ocirc;me de lave allong&eacute; qui se forme g&eacute;n&eacute;ralement sous la forme d&amp;#039;une lave &agrave; haute silice &eacute;clate sur le flanc abrupt d&amp;#039;un volcan. L&amp;#039;axe du d&ocirc;me perpendiculaire &agrave; la pente du volcan est plus court que l&amp;#039;axe parall&egrave;le &agrave; la pente, cr&eacute;ant une forme elliptique. Le bord d&amp;#039;attaque de la coul&eacute;e est souvent bloc et escarp&eacute;.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/coulee-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>coul&eacute;e<\/a> de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;LAVE&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Terme g&eacute;n&eacute;ral d&eacute;signant le magma (roche en fusion) qui a fait &eacute;ruption &agrave; la surface de la Terre et qui conserve son int&eacute;grit&eacute; sous forme de masse fluide ou visqueuse, plut&ocirc;t que d&amp;#039;exploser en fragments.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/lave-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>lave<\/a> active est repr&eacute;sent&eacute;e dans des tons de jaune et d&rsquo;orange, et s&rsquo;&eacute;tend vers le sud &agrave; partir de l&rsquo;<a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;&Eacute;VENT&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;div&amp;gt;Toute ouverture &agrave; la surface de la Terre par laquelle le magma entre en &eacute;ruption ou les gaz volcaniques sont &eacute;mis.&amp;lt;\/div&amp;gt;&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/event-fr\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>&eacute;vent<\/a>. De minces d&eacute;p&ocirc;ts de cendres volcaniques sont visibles sur la neige et la glace, sous forme de rayons radiaux qui se forment lorsque les cendres sont &eacute;mises sous l&rsquo;effet d&rsquo;un changement de direction du vent.<\/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":11142,"parent":11396,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-11792","page","type-page","status-publish","has-post-thumbnail","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/pages\/11792","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/users\/8"}],"replies":[{"embeddable":true,"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/comments?post=11792"}],"version-history":[{"count":0,"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/pages\/11792\/revisions"}],"up":[{"embeddable":true,"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/pages\/11396"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/media\/11142"}],"wp:attachment":[{"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/media?parent=11792"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}