{"id":57,"date":"2025-09-29T14:27:54","date_gmt":"2025-09-29T12:27:54","guid":{"rendered":"https:\/\/geops.geol.u-psud.fr\/pds\/?page_id=57"},"modified":"2025-12-02T16:47:38","modified_gmt":"2025-12-02T15:47:38","slug":"environnements-glaciaires","status":"publish","type":"page","link":"https:\/\/geops.geol.u-psud.fr\/pds\/environnements-glaciaires\/","title":{"rendered":"Environnements glaciaires"},"content":{"rendered":"<p><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-1 fusion-flex-container has-pattern-background has-mask-background nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"--awb-border-radius-top-left:0px;--awb-border-radius-top-right:0px;--awb-border-radius-bottom-right:0px;--awb-border-radius-bottom-left:0px;--awb-flex-wrap:wrap;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-flex-start fusion-flex-content-wrap\" style=\"max-width:1248px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-0 fusion_builder_column_1_2 1_2 fusion-flex-column\" style=\"--awb-padding-top:12%;--awb-padding-right:12%;--awb-padding-bottom:12%;--awb-padding-left:12%;--awb-bg-color:var(--awb-color1);--awb-bg-color-hover:var(--awb-color1);--awb-bg-size:cover;--awb-width-large:50%;--awb-margin-top-large:0px;--awb-spacing-right-large:3.84%;--awb-margin-bottom-large:0px;--awb-spacing-left-large:3.072%;--awb-width-medium:50%;--awb-order-medium:0;--awb-spacing-right-medium:3.84%;--awb-spacing-left-medium:3.072%;--awb-width-small:100%;--awb-order-small:0;--awb-spacing-right-small:1.92%;--awb-spacing-left-small:1.92%;\" data-scroll-devices=\"small-visibility,medium-visibility,large-visibility\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\"><div class=\"fusion-title title fusion-title-1 fusion-sep-none fusion-title-text fusion-title-size-two\" style=\"--awb-margin-top-small:10px;--awb-margin-right-small:0px;--awb-margin-bottom-small:10px;--awb-margin-left-small:0px;\"><h2 class=\"fusion-title-heading title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:46;line-height:var(--awb-typography1-line-height);\">Environnements glaciaires<\/h2><\/div><\/div><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-1 fusion_builder_column_1_2 1_2 fusion-flex-column\" style=\"--awb-bg-size:cover;--awb-width-large:50%;--awb-margin-top-large:0px;--awb-spacing-right-large:3.84%;--awb-margin-bottom-large:20px;--awb-spacing-left-large:3.84%;--awb-width-medium:50%;--awb-order-medium:0;--awb-spacing-right-medium:3.84%;--awb-spacing-left-medium:3.84%;--awb-width-small:100%;--awb-order-small:0;--awb-spacing-right-small:1.92%;--awb-spacing-left-small:1.92%;\" data-scroll-devices=\"small-visibility,medium-visibility,large-visibility\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\"><div class=\"fusion-image-element \" style=\"--awb-caption-title-font-family:var(--h2_typography-font-family);--awb-caption-title-font-weight:var(--h2_typography-font-weight);--awb-caption-title-font-style:var(--h2_typography-font-style);--awb-caption-title-size:var(--h2_typography-font-size);--awb-caption-title-transform:var(--h2_typography-text-transform);--awb-caption-title-line-height:var(--h2_typography-line-height);--awb-caption-title-letter-spacing:var(--h2_typography-letter-spacing);\"><span class=\" fusion-imageframe imageframe-none imageframe-1 hover-type-none\"><img decoding=\"async\" width=\"605\" height=\"453\" title=\"environnement glaciere\" src=\"https:\/\/geops.geol.u-psud.fr\/pds\/wp-content\/uploads\/sites\/3\/2025\/09\/environnement-glaciere.jpg\" alt class=\"img-responsive wp-image-58\" srcset=\"https:\/\/geops.geol.u-psud.fr\/pds\/wp-content\/uploads\/sites\/3\/2025\/09\/environnement-glaciere-200x150.jpg 200w, https:\/\/geops.geol.u-psud.fr\/pds\/wp-content\/uploads\/sites\/3\/2025\/09\/environnement-glaciere-400x300.jpg 400w, https:\/\/geops.geol.u-psud.fr\/pds\/wp-content\/uploads\/sites\/3\/2025\/09\/environnement-glaciere-600x449.jpg 600w, https:\/\/geops.geol.u-psud.fr\/pds\/wp-content\/uploads\/sites\/3\/2025\/09\/environnement-glaciere.jpg 605w\" sizes=\"(max-width: 640px) 100vw, 600px\" \/><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-2 fusion-flex-container has-pattern-background has-mask-background nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"--awb-border-radius-top-left:0px;--awb-border-radius-top-right:0px;--awb-border-radius-bottom-right:0px;--awb-border-radius-bottom-left:0px;--awb-flex-wrap:wrap;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-flex-start fusion-flex-content-wrap\" style=\"max-width:1248px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-2 fusion_builder_column_1_1 1_1 fusion-flex-column\" style=\"--awb-bg-size:cover;--awb-width-large:100%;--awb-margin-top-large:0px;--awb-spacing-right-large:1.92%;--awb-margin-bottom-large:20px;--awb-spacing-left-large:1.92%;--awb-width-medium:100%;--awb-order-medium:0;--awb-spacing-right-medium:1.92%;--awb-spacing-left-medium:1.92%;--awb-width-small:100%;--awb-order-small:0;--awb-spacing-right-small:1.92%;--awb-spacing-left-small:1.92%;\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\"><div class=\"fusion-text fusion-text-1\"><p>Les cons\u00e9quences du changement climatique sont particuli\u00e8rement importantes dans les environnements de hautes latitudes, o\u00f9 les glaciers, la couverture neigeuse et le perg\u00e9lisol disparaissent \u00e0 un rythme alarmant. Ces changements rapides affectent les processus de surface, avec des cons\u00e9quences relativement m\u00e9connues pour les risques naturels. C\u2019est notamment le cas des crues glaciaires (Glacial Lake Outburst Floods; GLOFs) qui r\u00e9sultent de la vidange de lacs glaciaires suite \u00e0 la rupture d\u2019une moraine ou d\u2019un barrage de glace..<\/p>\n<\/div><div class=\"fusion-text fusion-text-2\"><p><strong>Objectifs du Th\u00e8me\u00a0:<\/strong> Nos activit\u00e9s de recherche ont pour but de reconstituer l&#8217;\u00e9volution des glaciers et des risques naturels associ\u00e9s durant l\u2019Holoc\u00e8ne, sur base d\u2019enregistrements s\u00e9dimentaires de fjords et de lacs.<\/p>\n<\/div><div class=\"fusion-text fusion-text-3\"><p><strong>Liste Permanents\/Non permanents\u00a0:<\/strong><\/p>\n<p>S. Bertrand, G. Siani, <span data-olk-copy-source=\"MessageBody\">G. Lyu<\/span><\/p>\n<\/div><\/div><\/div><\/div><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-3 fusion-flex-container has-pattern-background has-mask-background nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"--awb-border-radius-top-left:0px;--awb-border-radius-top-right:0px;--awb-border-radius-bottom-right:0px;--awb-border-radius-bottom-left:0px;--awb-flex-wrap:wrap;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-flex-start fusion-flex-content-wrap\" style=\"max-width:1248px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-3 fusion_builder_column_1_1 1_1 fusion-flex-column\" style=\"--awb-bg-size:cover;--awb-width-large:100%;--awb-margin-top-large:0px;--awb-spacing-right-large:1.92%;--awb-margin-bottom-large:20px;--awb-spacing-left-large:1.92%;--awb-width-medium:100%;--awb-order-medium:0;--awb-spacing-right-medium:1.92%;--awb-spacing-left-medium:1.92%;--awb-width-small:100%;--awb-order-small:0;--awb-spacing-right-small:1.92%;--awb-spacing-left-small:1.92%;\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\"><div class=\"fusion-separator fusion-full-width-sep\" style=\"align-self: center;margin-left: auto;margin-right: auto;margin-top:10px;margin-bottom:20px;width:100%;\"><div class=\"fusion-separator-border sep-single sep-solid\" style=\"--awb-height:20px;--awb-amount:20px;border-color:var(--awb-color3);border-top-width:1px;\"><\/div><\/div><div class=\"fusion-title title fusion-title-2 fusion-sep-none fusion-title-text fusion-title-size-two\" style=\"--awb-margin-top-small:10px;--awb-margin-right-small:0px;--awb-margin-bottom-small:10px;--awb-margin-left-small:0px;\"><h2 class=\"fusion-title-heading title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:46;line-height:var(--awb-typography1-line-height);\">Les projets<\/h2><\/div><div class=\"fusion-blog-shortcode fusion-blog-shortcode-1 fusion-blog-archive fusion-blog-layout-grid-wrapper fusion-blog-no fusion-no-small-visibility fusion-no-medium-visibility fusion-blog-no-images fusion-blog-layout-center\" style=\"--grid_separator_color:var(--awb-custom_color_1);\"><style type=\"text\/css\">.fusion-blog-shortcode-1 .fusion-blog-layout-grid .fusion-post-grid{padding:20px;}.fusion-blog-shortcode-1 .fusion-posts-container{margin-left: -20px !important; margin-right:-20px !important;}<\/style><div class=\"fusion-posts-container fusion-posts-container-no fusion-no-meta-info fusion-blog-layout-grid fusion-blog-layout-grid-3 isotope fusion-blog-equal-heights\" data-pages=\"1\" data-grid-col-space=\"40\" style=\"margin: -20px -20px 0;min-height:500px;\"><article id=\"blog-1-post-167\" class=\"fusion-post-grid post-167 post type-post status-publish format-standard hentry category-cycle-carbonne category-environnements-glaciaires\">\n<div class=\"fusion-post-wrapper\" style=\"background-color:rgba(255,255,255,0);border:1px solid var(--awb-color2);border-bottom-width:3px;\"><div class=\"fusion-post-content-wrapper\" style=\"padding:30px 30px 30px 30px;\"><div class=\"fusion-post-content post-content\"><h5 class=\"blog-shortcode-post-title entry-title\"><a href=\"https:\/\/geops.geol.u-psud.fr\/pds\/2025\/09\/29\/cpj-haute-latitudes\/\">CPJ haute latitudes<\/a><\/h5><\/div><\/div><div class=\"fusion-clearfix\"><\/div><\/div>\n<\/article>\n<article id=\"blog-1-post-192\" class=\"fusion-post-grid post-192 post type-post status-publish format-standard hentry category-environnements-glaciaires\">\n<div class=\"fusion-post-wrapper\" style=\"background-color:rgba(255,255,255,0);border:1px solid var(--awb-color2);border-bottom-width:3px;\"><div class=\"fusion-post-content-wrapper\" style=\"padding:30px 30px 30px 30px;\"><div class=\"fusion-post-content post-content\"><h5 class=\"blog-shortcode-post-title entry-title\"><a href=\"https:\/\/geops.geol.u-psud.fr\/pds\/2025\/09\/30\/climaglof\/\">CLIMAGLOF<\/a><\/h5><\/div><\/div><div class=\"fusion-clearfix\"><\/div><\/div>\n<\/article>\n<div class=\"fusion-clearfix\"><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/p>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-57","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/pages\/57","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/comments?post=57"}],"version-history":[{"count":4,"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/pages\/57\/revisions"}],"predecessor-version":[{"id":214,"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/pages\/57\/revisions\/214"}],"wp:attachment":[{"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/media?parent=57"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}