{"id":13831,"date":"2021-07-22T19:10:32","date_gmt":"2021-07-22T17:10:32","guid":{"rendered":"http:\/\/volcanx.cluster031.hosting.ovh.net\/?post_type=glossary&#038;p=13831"},"modified":"2021-07-26T17:20:46","modified_gmt":"2021-07-26T15:20:46","slug":"dome-resurgence-fr","status":"publish","type":"glossary","link":"https:\/\/volcanofoundation.org\/fr\/glossary\/dome-resurgence-fr\/","title":{"rendered":"D\u00d4ME R\u00c9SURGENCE"},"content":{"rendered":"<div>Les hautes terres centrales de nombreuses grandes caldeiras form&eacute;es par la <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;D&Eacute;FORMATION&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Changements &agrave; la surface d&amp;#039;un volcan qui se produisent en raison du mouvement du magma sous la surface. La plupart des d&eacute;formations volcaniques ne peuvent &ecirc;tre d&eacute;tect&eacute;es et mesur&eacute;es qu&amp;#039;&agrave; l&amp;#039;aide de techniques d&amp;#039;arpentage pr&eacute;cises telles qu&amp;#039;un syst&egrave;me de positionnement mondial (GPS), un tiltm&egrave;tre, un radar d&amp;#039;ouverture synth&eacute;tique interf&eacute;rom&eacute;trique (InSAR) ou un distancem&egrave;tre &eacute;lectronique (EDM).&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/deformation-fr\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">d&eacute;formation<\/a> progressive du plancher de la <a class=\"glossary\" title=\"Grande d&eacute;pression volcanique en forme de bassin d'un diam&egrave;tre beaucoup plus grand que les volcaniques inclus ; peut varier de 2 &agrave; 50 km de diam&egrave;tre.\" href=\"https:\/\/volcanoes.usgs.gov\/vsc\/glossary\/caldera.html\">caldeira <\/a>apr&egrave;s l&rsquo;effondrement de la caldeira &agrave; la suite d&rsquo;une nouvelle intrusion <a class=\"glossary\" title=\"Roche fondue sous la surface de la Terre.\" href=\"https:\/\/volcanoes.usgs.gov\/vsc\/glossary\/magma.html\">magmatique<\/a>.<\/div>\n","protected":false},"excerpt":{"rendered":"<p>Les hautes terres centrales de nombreuses grandes caldeiras form&eacute;es par la <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;D&Eacute;FORMATION&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Changements &agrave; la surface d&amp;#039;un volcan qui se produisent en raison du mouvement du magma sous la surface. La plupart des d&eacute;formations volcaniques ne peuvent &ecirc;tre d&eacute;tect&eacute;es et mesur&eacute;es qu&amp;#039;&agrave; l&amp;#039;aide de techniques d&amp;#039;arpentage pr&eacute;cises telles qu&amp;#039;un syst&egrave;me de positionnement mondial (GPS), un tiltm&egrave;tre, un radar d&amp;#039;ouverture synth&eacute;tique interf&eacute;rom&eacute;trique (InSAR) ou un distancem&egrave;tre &eacute;lectronique (EDM).&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/fr\/glossary\/deformation-fr\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">d&eacute;formation<\/a> progressive du plancher de la caldeira apr&egrave;s l&rsquo;effondrement de la caldeira &agrave; la suite d&rsquo;une nouvelle intrusion magmatique.<\/p>\n","protected":false},"author":8,"featured_media":0,"menu_order":0,"template":"","meta":{"footnotes":""},"class_list":["post-13831","glossary","type-glossary","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/glossary\/13831","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/glossary"}],"about":[{"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/types\/glossary"}],"author":[{"embeddable":true,"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/users\/8"}],"version-history":[{"count":0,"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/glossary\/13831\/revisions"}],"wp:attachment":[{"href":"https:\/\/volcanofoundation.org\/fr\/wp-json\/wp\/v2\/media?parent=13831"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}