{"id":1797,"date":"2024-06-14T12:26:53","date_gmt":"2024-06-14T10:26:53","guid":{"rendered":"https:\/\/hydrography.boku.ac.at\/wordpress\/?page_id=1797"},"modified":"2025-01-28T14:37:57","modified_gmt":"2025-01-28T13:37:57","slug":"info-panel-04","status":"publish","type":"page","link":"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/info-panel-04\/","title":{"rendered":"Info Panel 04"},"content":{"rendered":"
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\n\t\t\t\n\t\t\t<\/i>\t\t\t<\/a>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t
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WHY IS THE <\/span> BEAUTIFUL LAKE ALTAUSSEE<\/span><\/h2>\t\t\t\t\t

situated deep between high mountains like Loser Sandling and Trisselwand?<\/p><\/span>\n\t\t\t\t\t\t\t\t\t<\/i><\/span>\t\t\t\t\t\t\t<\/div>\n\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t

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\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\"BOKU_University\"\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
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The story starts in the ocean, where tropical reefs grew in shallow water hundreds of millions of years ago (Loser summit). Long before that, salt layers were left behind from prehistoric seas that dried out on hot coastlines, eventually forming the mountains (Sandling) and carbonates deposited on the ocean floor (Trisselwand). Later, Africa pushed these rocks onto the southern edge of Europe and created a mountain belt – the Alps. Soon after, rivers developed (like the Enns river) and cut deep valleys into the plateaus of the still young Alps.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t

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Glacier Ice on the top of mountains<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
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Later, glaciers flooded these mountains and eroded them during the penultimate glaciation, with up to 1,000 m deep holes which were refilled by rivers like the Enns. During the last glaciation, ice from the plateau of the Totes Gebirge streamed through the valley.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t

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Glacier Ice on the top of mountains<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
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As the ice melted, several lakes developed and the recent Lake Altaussee was formed by the Augstbach alluvial fan, landslides from the slopes, and lake sediments.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Modern glacier and proglactial lake are analogue to Lake Altaussee during glacial retreat<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
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\n\t\t\t\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
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back <\/span> to the Panel Overview<\/span><\/h4>\t\t\t\t\t<\/i><\/span>\t\t\t\t\t\t\t<\/div>\n\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>","protected":false},"excerpt":{"rendered":"

WHY IS THE BEAUTIFUL LAKE ALTAUSSEE situated deep between high mountains like Loser Sandling and Trisselwand? The story starts in the ocean, where tropical reefs grew in shallow water hundreds of millions of years ago (Loser summit). Long before that, salt layers were left behind from prehistoric seas that dried out on hot coastlines, eventually […]<\/p>\n","protected":false},"author":3,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"elementor_canvas","meta":{"ocean_post_layout":"","ocean_both_sidebars_style":"","ocean_both_sidebars_content_width":0,"ocean_both_sidebars_sidebars_width":0,"ocean_sidebar":"","ocean_second_sidebar":"","ocean_disable_margins":"enable","ocean_add_body_class":"","ocean_shortcode_before_top_bar":"","ocean_shortcode_after_top_bar":"","ocean_shortcode_before_header":"","ocean_shortcode_after_header":"","ocean_has_shortcode":"","ocean_shortcode_after_title":"","ocean_shortcode_before_footer_widgets":"","ocean_shortcode_after_footer_widgets":"","ocean_shortcode_before_footer_bottom":"","ocean_shortcode_after_footer_bottom":"","ocean_display_top_bar":"default","ocean_display_header":"default","ocean_header_style":"","ocean_center_header_left_menu":"","ocean_custom_header_template":"","ocean_custom_logo":0,"ocean_custom_retina_logo":0,"ocean_custom_logo_max_width":0,"ocean_custom_logo_tablet_max_width":0,"ocean_custom_logo_mobile_max_width":0,"ocean_custom_logo_max_height":0,"ocean_custom_logo_tablet_max_height":0,"ocean_custom_logo_mobile_max_height":0,"ocean_header_custom_menu":"","ocean_menu_typo_font_family":"","ocean_menu_typo_font_subset":"","ocean_menu_typo_font_size":0,"ocean_menu_typo_font_size_tablet":0,"ocean_menu_typo_font_size_mobile":0,"ocean_menu_typo_font_size_unit":"px","ocean_menu_typo_font_weight":"","ocean_menu_typo_font_weight_tablet":"","ocean_menu_typo_font_weight_mobile":"","ocean_menu_typo_transform":"","ocean_menu_typo_transform_tablet":"","ocean_menu_typo_transform_mobile":"","ocean_menu_typo_line_height":0,"ocean_menu_typo_line_height_tablet":0,"ocean_menu_typo_line_height_mobile":0,"ocean_menu_typo_line_height_unit":"","ocean_menu_typo_spacing":0,"ocean_menu_typo_spacing_tablet":0,"ocean_menu_typo_spacing_mobile":0,"ocean_menu_typo_spacing_unit":"","ocean_menu_link_color":"","ocean_menu_link_color_hover":"","ocean_menu_link_color_active":"","ocean_menu_link_background":"","ocean_menu_link_hover_background":"","ocean_menu_link_active_background":"","ocean_menu_social_links_bg":"","ocean_menu_social_hover_links_bg":"","ocean_menu_social_links_color":"","ocean_menu_social_hover_links_color":"","ocean_disable_title":"default","ocean_disable_heading":"default","ocean_post_title":"","ocean_post_subheading":"","ocean_post_title_style":"","ocean_post_title_background_color":"","ocean_post_title_background":0,"ocean_post_title_bg_image_position":"","ocean_post_title_bg_image_attachment":"","ocean_post_title_bg_image_repeat":"","ocean_post_title_bg_image_size":"","ocean_post_title_height":0,"ocean_post_title_bg_overlay":0.5,"ocean_post_title_bg_overlay_color":"","ocean_disable_breadcrumbs":"default","ocean_breadcrumbs_color":"","ocean_breadcrumbs_separator_color":"","ocean_breadcrumbs_links_color":"","ocean_breadcrumbs_links_hover_color":"","ocean_display_footer_widgets":"default","ocean_display_footer_bottom":"default","ocean_custom_footer_template":"","footnotes":""},"class_list":["post-1797","page","type-page","status-publish","hentry","entry"],"_links":{"self":[{"href":"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/wp-json\/wp\/v2\/pages\/1797","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/wp-json\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/wp-json\/wp\/v2\/comments?post=1797"}],"version-history":[{"count":10,"href":"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/wp-json\/wp\/v2\/pages\/1797\/revisions"}],"predecessor-version":[{"id":2101,"href":"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/wp-json\/wp\/v2\/pages\/1797\/revisions\/2101"}],"wp:attachment":[{"href":"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/wp-json\/wp\/v2\/media?parent=1797"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}