{"id":11594,"date":"2021-07-14T12:32:35","date_gmt":"2021-07-14T10:32:35","guid":{"rendered":"http:\/\/volcanx.cluster031.hosting.ovh.net\/?page_id=11594"},"modified":"2021-10-04T18:31:57","modified_gmt":"2021-10-04T16:31:57","slug":"deformacion","status":"publish","type":"page","link":"https:\/\/volcanofoundation.org\/es\/creando-conocimiento-de-los-riesgos\/monitorizacion\/deformacion\/","title":{"rendered":"DEFORMACI\u00d3N"},"content":{"rendered":"<div id=\"av_section_1\" class=\"avia-section av-85tvrm-3e95231a7b3e6eb192907f404f41a286 main_color avia-section-default avia-no-border-styling  avia-builder-el-0  el_before_av_section  avia-builder-el-first  avia-full-stretch av-parallax-section avia-bg-style-parallax av-minimum-height av-minimum-height-25 av-height-25  container_wrap fullsize\" data-section-bg-repeat=\"stretch\" data-av_minimum_height_pc=\"25\" data-av_min_height_opt=\"25\"><div class=\"av-parallax\" data-avia-parallax-ratio=\"0.3\"><div class=\"av-parallax-inner main_color avia-full-stretch\"><\/div><\/div><div class=\"container av-section-cont-open\"><main role=\"main\" itemprop=\"mainContentOfPage\" class=\"template-page content  av-content-full alpha units\"><div class=\"post-entry post-entry-type-page post-entry-11594\"><div class=\"entry-content-wrapper clearfix\">\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-377mki-891bdcf97286948f143384db57d78c91\">\n.flex_column.av-377mki-891bdcf97286948f143384db57d78c91{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-377mki-891bdcf97286948f143384db57d78c91 av_one_fifth  avia-builder-el-1  el_before_av_three_fifth  avia-builder-el-first  first flex_column_div av-zero-column-padding  \"><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-44v1oi-4270c45783cf4dfabc2e0046b5bfca7a\">\n.flex_column.av-44v1oi-4270c45783cf4dfabc2e0046b5bfca7a{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-44v1oi-4270c45783cf4dfabc2e0046b5bfca7a av_three_fifth  avia-builder-el-2  el_after_av_one_fifth  el_before_av_one_fifth  flex_column_div av-zero-column-padding  \"><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-2wneaq-c7141c0f93804d3dc6134a419c02967d\">\n#top .av_textblock_section.av-2wneaq-c7141c0f93804d3dc6134a419c02967d .avia_textblock{\ncolor:#ffffff;\n}\n<\/style>\n<section class=\"av_textblock_section av-2wneaq-c7141c0f93804d3dc6134a419c02967d \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock av_inherit_color\" itemprop=\"text\"><div class=\"h2-cinta-programas\">\n<h2 style=\"text-align: center; font-size: 2.5em;\">CREAR CONOCIMIENTO DE LOS RIESGOS<\/h2>\n<\/div>\n<\/div><\/section><br>\n<section class=\"av_textblock_section av-2wneaq-34462baf835e0e88628f9f1fcf41a06e \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p class=\"p-cinta-programas\" style=\"text-align: center; background: #f5312a !important;\">&iquest;POR QU&Eacute; NACI&Oacute; LA FUNDACI&Oacute;N?<span class=\"flecha-donativo\" style=\"vertical-align: inherit;\"> &gt;<\/span><\/p>\n<\/div><\/section><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-377mki-fc3240a24cacc3f72868647236f26abd\">\n.flex_column.av-377mki-fc3240a24cacc3f72868647236f26abd{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-377mki-fc3240a24cacc3f72868647236f26abd av_one_fifth  avia-builder-el-5  el_after_av_three_fifth  avia-builder-el-last  flex_column_div av-zero-column-padding  \"><\/div><\/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-11594\"><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\">Los desastres no son naturales<\/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 a las sociedades vulnerables. El conocimiento ayuda a reducir la vulnerabilidad social y estructural para tener sociedades m&aacute;s resilientes!<\/p>\n<\/blockquote>\n<\/div><\/section><\/div><\/div><!--close column table wrapper. Autoclose: 1 --><\/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-11594\"><div class=\"entry-content-wrapper clearfix\"><section class=\"av_textblock_section av-kqt9jd5e-cd33964ef4e3b772df7fef522b816d29 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><div class=\"panel-pane pane-node-title\">\n<div class=\"pane-content\">\n<h2>El movimiento en la superficie proporciona informaci&oacute;n sobre el subsuelo<\/h2>\n<\/div>\n<\/div>\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>La deformaci&oacute;n se produce por la inflaci&oacute;n de un dep&oacute;sito de magma y una intrusi&oacute;n<\/h3>\n<p>Las deformaciones superficiales proporcionan informaci&oacute;n importante sobre la estructura interna y el funcionamiento de los volcanes. Cada erupci&oacute;n est&aacute; precedida por un lento hinchamiento (inflaci&oacute;n) del volc&aacute;n y una r&aacute;pida deflaci&oacute;n durante la erupci&oacute;n. <strong>La principal fuente de <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;DEFORMACI&Oacute;N&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Cambios en la superficie de un volc&aacute;n que se producen debido al movimiento del magma debajo de la superficie. La mayor&iacute;a de las deformaciones volc&aacute;nicas solo se pueden detectar y medir con t&eacute;cnicas de topograf&iacute;a precisas, como un sistema de posicionamiento global (GPS), un medidor de inclinaci&oacute;n, un radar de apertura sint&eacute;tica interferom&eacute;trica (InSAR) o un medidor de distancia electr&oacute;nico (EDM).&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/deformacion-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">deformaci&oacute;n<\/a> es magn&eacute;tica<\/strong>.<\/p>\n<\/div><\/section><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-kqta1i5b-a345f9d882c51d4089993cf6d16e9b60\">\n#top .hr.hr-invisible.av-kqta1i5b-a345f9d882c51d4089993cf6d16e9b60{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-kqta1i5b-a345f9d882c51d4089993cf6d16e9b60 hr-invisible  avia-builder-el-13  el_after_av_textblock  el_before_av_textblock \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div><br>\n<section class=\"av_textblock_section av-kqtdsfvd-d152eb0e3d3e094fcc403a1e69a26b44 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><h3>Monitoreo de la deformaci&oacute;n<\/h3>\n<p>Los cambios en la <strong>superficie del suelo<\/strong> de un volc&aacute;n (<a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;DEFORMACI&Oacute;N&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Cambios en la superficie de un volc&aacute;n que se producen debido al movimiento del magma debajo de la superficie. La mayor&iacute;a de las deformaciones volc&aacute;nicas solo se pueden detectar y medir con t&eacute;cnicas de topograf&iacute;a precisas, como un sistema de posicionamiento global (GPS), un medidor de inclinaci&oacute;n, un radar de apertura sint&eacute;tica interferom&eacute;trica (InSAR) o un medidor de distancia electr&oacute;nico (EDM).&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/deformacion-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">deformaci&oacute;n<\/a> volc&aacute;nica) aparecen como hinchaz&oacute;n, hundimiento o agrietamiento, que pueden ser causados por el <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;MAGMA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Roca fundida bajo la superficie de la Tierra.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/magma-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>magma<\/a>, el gas u otros fluidos (normalmente agua) que se mueven en el subsuelo o por los movimientos de la <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;CORTEZA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;La corteza es la capa principal m&aacute;s externa de la tierra, que oscila entre unos 10 y 65 km de espesor en todo el mundo. Los 15-35 km m&aacute;s altos de corteza son lo suficientemente fr&aacute;giles como para producir terremotos.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/corteza-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>corteza<\/a> terrestre debido al movimiento a lo largo de las fallas. A menudo, esta <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;DEFORMACI&Oacute;N&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Cambios en la superficie de un volc&aacute;n que se producen debido al movimiento del magma debajo de la superficie. La mayor&iacute;a de las deformaciones volc&aacute;nicas solo se pueden detectar y medir con t&eacute;cnicas de topograf&iacute;a precisas, como un sistema de posicionamiento global (GPS), un medidor de inclinaci&oacute;n, un radar de apertura sint&eacute;tica interferom&eacute;trica (InSAR) o un medidor de distancia electr&oacute;nico (EDM).&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/deformacion-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">deformaci&oacute;n<\/a> es muy peque&ntilde;a en magnitud -unos pocos cent&iacute;metros (pulgadas) o menos- y, por lo tanto, s&oacute;lo puede ser detectada y <a title=\"60% DE LOS VOLCANES ACTIVOS NO TIENEN SISTEMA DE MONITORIZACI&Oacute;N\" href=\"http:\/\/volcanx.cluster031.hosting.ovh.net\/fr\/most-of-active-volcanoes-have-no-monitoring-system\/\">monitorizada<\/a> con instrumentos muy sensibles.<\/p>\n<\/div><\/section><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-1be8acw-edad6df5b24231d2c407a1b98d1fe3f4\">\n#top .hr.hr-invisible.av-1be8acw-edad6df5b24231d2c407a1b98d1fe3f4{\nheight:20px;\n}\n<\/style>\n<div class=\"hr av-1be8acw-edad6df5b24231d2c407a1b98d1fe3f4 hr-invisible  avia-builder-el-15  el_after_av_textblock  el_before_av_textblock \"><span class=\"hr-inner \"><span class=\"hr-inner-style\"><\/span><\/span><\/div><br>\n<section class=\"av_textblock_section av-kqterpr6-f6dbcd07f29ed0b44fd4c06a6ac45a70 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><h3>&iquest;C&oacute;mo se controla la deformaci&oacute;n?<\/h3>\n<p>El <a href=\"http:\/\/www.usgs.gov\">Programa de Riesgo Volc&aacute;nico<\/a> instala y mantiene redes de instrumentos alrededor de los volcanes para controlar los cambios en la superficie terrestre a lo largo del tiempo. Las mediciones terrestres se realizan en puntos concretos de la superficie terrestre mediante receptores del <strong>Sistema de Posicionamiento Global (GPS)<\/strong>. Las observaciones espaciales de gran superficie se realizan con tecnolog&iacute;as de sat&eacute;lite como <strong>InSAR<\/strong>. Combinando estos datos con otras t&eacute;cnicas de vigilancia (observaciones geol&oacute;gicas, detecci&oacute;n de terremotos y de gases), los cient&iacute;ficos pueden comprender mejor lo que ocurre bajo el suelo, saber cu&aacute;ndo un volc&aacute;n se comporta fuera de &laquo;contexto&raquo; y avisar cuando un volc&aacute;n muestra signos de erupci&oacute;n.<\/p>\n<\/div><\/section><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-1iz7j36-2c9786a9f3f90bd1396461500bfb925f\">\n.flex_column.av-1iz7j36-2c9786a9f3f90bd1396461500bfb925f{\nborder-radius:0px 0px 0px 0px;\npadding:0px 0px 0px 0px;\n}\n<\/style>\n<div class=\"flex_column av-1iz7j36-2c9786a9f3f90bd1396461500bfb925f av_two_fifth  avia-builder-el-17  el_after_av_three_fifth  avia-builder-el-last  flex_column_div av-zero-column-padding  \"><p>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-kqtcpnnn-0591d41066c4ad030b98f175929c053e\">\n.avia-image-container.av-kqtcpnnn-0591d41066c4ad030b98f175929c053e img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-kqtcpnnn-0591d41066c4ad030b98f175929c053e .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<\/p><div class=\"avia-image-container av-kqtcpnnn-0591d41066c4ad030b98f175929c053e 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-11600 avia-img-lazy-loading-not-11600 avia_image \" src=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/bulge-mount-st-helens.jpg\" alt=\"\" title=\"bulge-mount-st-helens\" height=\"757\" width=\"1140\" itemprop=\"thumbnailUrl\" srcset=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/bulge-mount-st-helens.jpg 1140w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/bulge-mount-st-helens-300x199.jpg 300w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/bulge-mount-st-helens-1030x684.jpg 1030w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/bulge-mount-st-helens-768x510.jpg 768w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/bulge-mount-st-helens-705x468.jpg 705w\" sizes=\"(max-width: 1140px) 100vw, 1140px\"\/><\/div><\/div><\/div><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-kqtcpuh7-d8db4528b4900c045b62972c54904769\">\n#top .av_textblock_section.av-kqtcpuh7-d8db4528b4900c045b62972c54904769 .avia_textblock{\nfont-size:14px;\n}\n<\/style>\n<section class=\"av_textblock_section av-kqtcpuh7-d8db4528b4900c045b62972c54904769 \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p><em>La protuberancia en el lado norte del Monte St. Helens se desarroll&oacute; a medida que el <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;MAGMA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Roca fundida bajo la superficie de la Tierra.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/magma-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>magma<\/a> fue empujado hacia arriba dentro del pico antes del 18 de mayo de 1980. Vista desde el noreste.<\/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  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-kqte8z1i-9748e454200afecd31ebfa61393d3efd\">\n.avia-image-container.av-kqte8z1i-9748e454200afecd31ebfa61393d3efd img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-kqte8z1i-9748e454200afecd31ebfa61393d3efd .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div class=\"avia-image-container av-kqte8z1i-9748e454200afecd31ebfa61393d3efd av-styling- avia-align-center  avia-builder-el-21  el_after_av_hr  el_before_av_textblock \" itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\"><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><img decoding=\"async\" fetchpriority=\"high\" class=\"wp-image-11604 avia-img-lazy-loading-not-11604 avia_image \" src=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/temporary-gps-station-three-sisters.jpg\" alt=\"\" title=\"temporary-gps-station-three-sisters\" height=\"855\" width=\"1140\" itemprop=\"thumbnailUrl\" srcset=\"https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/temporary-gps-station-three-sisters.jpg 1140w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/temporary-gps-station-three-sisters-300x225.jpg 300w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/temporary-gps-station-three-sisters-1030x773.jpg 1030w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/temporary-gps-station-three-sisters-768x576.jpg 768w, https:\/\/volcanofoundation.org\/wp-content\/uploads\/2021\/07\/temporary-gps-station-three-sisters-705x529.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-kqte9kjf-e9bd2fbd3f9a53efca04f8d49e32eaaa\">\n#top .av_textblock_section.av-kqte9kjf-e9bd2fbd3f9a53efca04f8d49e32eaaa .avia_textblock{\nfont-size:14px;\n}\n<\/style>\n<section class=\"av_textblock_section av-kqte9kjf-e9bd2fbd3f9a53efca04f8d49e32eaaa \" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\"><div class=\"avia_textblock\" itemprop=\"text\"><p><em>Estaciones GPS temporales recogen datos para analizar la <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;DEFORMACI&Oacute;N&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Cambios en la superficie de un volc&aacute;n que se producen debido al movimiento del magma debajo de la superficie. La mayor&iacute;a de las deformaciones volc&aacute;nicas solo se pueden detectar y medir con t&eacute;cnicas de topograf&iacute;a precisas, como un sistema de posicionamiento global (GPS), un medidor de inclinaci&oacute;n, un radar de apertura sint&eacute;tica interferom&eacute;trica (InSAR) o un medidor de distancia electr&oacute;nico (EDM).&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/deformacion-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">deformaci&oacute;n<\/a> de la zona en Three Sisters, Oreg&oacute;n.<\/em><\/p>\n<\/div><\/section><br>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-q980xc-50f7dd054b06f60518f9b118b6077c50\">\n#top .hr.hr-invisible.av-q980xc-50f7dd054b06f60518f9b118b6077c50{\nheight:30px;\n}\n<\/style>\n<div class=\"hr av-q980xc-50f7dd054b06f60518f9b118b6077c50 hr-invisible  avia-builder-el-23  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>Deformation monitoring has two complementary functions, real-time status and internal geometric modelling.<\/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-11594","page","type-page","status-publish","has-post-thumbnail","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/pages\/11594","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=11594"}],"version-history":[{"count":0,"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/pages\/11594\/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=11594"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}