{"id":245,"date":"2026-03-24T11:19:44","date_gmt":"2026-03-24T10:19:44","guid":{"rendered":"https:\/\/geops.geol.u-psud.fr\/pds\/?page_id=245"},"modified":"2026-03-24T11:20:47","modified_gmt":"2026-03-24T10:20:47","slug":"glacial-environments","status":"publish","type":"page","link":"https:\/\/geops.geol.u-psud.fr\/pds\/en\/glacial-environments\/","title":{"rendered":"Glacial environments"},"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);\">Glacial environments<\/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>The consequences of climate change are particularly significant in high-latitude environments, where glaciers, snow cover and permafrost are disappearing at an alarming rate. These rapid changes affect surface processes, with consequences for natural hazards that are relatively poorly understood. This is particularly the case with glacial lake outburst floods (GLOFs), which result from the draining of glacial lakes following the breach of a moraine or ice dam.<\/p>\n<\/div><div class=\"fusion-text fusion-text-2\"><p><b>Aims of the research theme:<\/b> Our research aims to reconstruct the evolution of glaciers and associated natural hazards during the Holocene, based on sedimentary records from fjords and lakes.<\/p>\n<\/div><div class=\"fusion-text fusion-text-3\"><p><strong>List of permanent and non-permanent staff:<\/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);\">Projects<\/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-271\" class=\"fusion-post-grid post-271 post type-post status-publish format-standard hentry category-carbon-cycle category-glacial-environments\">\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\/en\/2026\/03\/26\/cpj-high-latitudes\/\">CPJ High Latitudes<\/a><\/h5><\/div><\/div><div class=\"fusion-clearfix\"><\/div><\/div>\n<\/article>\n<article id=\"blog-1-post-255\" class=\"fusion-post-grid post-255 post type-post status-publish format-standard hentry category-glacial-environments\">\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\/en\/2026\/03\/26\/climaglof-en\/\">CLIMAGLOF (EN)<\/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-245","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/pages\/245","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=245"}],"version-history":[{"count":2,"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/pages\/245\/revisions"}],"predecessor-version":[{"id":247,"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/pages\/245\/revisions\/247"}],"wp:attachment":[{"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/media?parent=245"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}