{"id":1806,"date":"2024-06-14T12:32:06","date_gmt":"2024-06-14T10:32:06","guid":{"rendered":"https:\/\/hydrography.boku.ac.at\/wordpress\/?page_id=1806"},"modified":"2025-01-28T14:30:06","modified_gmt":"2025-01-28T13:30:06","slug":"info-panel-05","status":"publish","type":"page","link":"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/info-panel-05\/","title":{"rendered":"Info Panel 05"},"content":{"rendered":"
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LAKE ALTAUSSEE<\/span> AS A TIME MACHINE<\/span><\/h2>\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\"UIBK_Logo\"\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 HISTORY OF THE LAKE LIES IN THE LAKE MUD<\/h1>

After the last glaciation around 15,000 years Before Common Era (BCE), the W\u00fcrmian glaciers formed a natural dam (end moraine) as they retreated, allowing the emergence of Lake Altaussee from the meltwater. At times, its water level was higher than today and the Altaussee community would have been submerged until prehistory. Later, the water level dropped up to 20 meters below the current level. Lake Altaussee finally rose to its current level when multiple debris flows
blocked the prehistoric outflow.<\/p>

Im Hochmittelalter, etwa um 800 n. Chr., ereigneten sich im Osten des Sees mehrere gro\u00dfe Felsst\u00fcrze mit insgesamt \u00fcber 300.000 m\u00b3 an Schutt, Ger\u00f6ll und Felsbl\u00f6cken. Am Seeboden sind daher Steinbl\u00f6cke mit \u00fcber 10 m H\u00f6he und 80 m Breite auffindbar.During the High Medieval, around 800 AD, several rockfalls occurred at the east end of the lake, totaling over 300,000 m\u00b3 of debris, rocks, and boulders. Boulders over 10 m high and 80 m wide can be found on the lake bottom.<\/p>

Around 1,100 AD, the Augstbach flowed into Lake Altaussee and was diverted into the Altausseer Traun by human intervention 200 years later.<\/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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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":"

LAKE ALTAUSSEE AS A TIME MACHINE THE HISTORY OF THE LAKE LIES IN THE LAKE MUD After the last glaciation around 15,000 years Before Common Era (BCE), the W\u00fcrmian glaciers formed a natural dam (end moraine) as they retreated, allowing the emergence of Lake Altaussee from the meltwater. At times, its water level was higher […]<\/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-1806","page","type-page","status-publish","hentry","entry"],"_links":{"self":[{"href":"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/wp-json\/wp\/v2\/pages\/1806","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=1806"}],"version-history":[{"count":16,"href":"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/wp-json\/wp\/v2\/pages\/1806\/revisions"}],"predecessor-version":[{"id":2086,"href":"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/wp-json\/wp\/v2\/pages\/1806\/revisions\/2086"}],"wp:attachment":[{"href":"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/wp-json\/wp\/v2\/media?parent=1806"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}