{"id":1285,"date":"2025-10-07T10:40:59","date_gmt":"2025-10-07T10:40:59","guid":{"rendered":"https:\/\/icewalk.it\/gletschertoepfe\/"},"modified":"2026-01-26T10:19:25","modified_gmt":"2026-01-26T10:19:25","slug":"gletschertoepfe","status":"publish","type":"page","link":"https:\/\/icewalk.it\/de\/gletschertoepfe\/","title":{"rendered":"Gletschert\u00f6pfe"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8220;1&#8243; _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; custom_padding=&#8220;||100px|||&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_row column_structure=&#8220;3_5,2_5&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; width=&#8220;100%&#8220; custom_padding=&#8220;|20px|2%|20px|false|false&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_column type=&#8220;3_5&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_text _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; text_font=&#8220;&#8211;et_global_body_font|700|||||||&#8220; header_font=&#8220;&#8211;et_global_heading_font||||||||&#8220; header_text_color=&#8220;gcid-f5853230-0d63-4130-b142-81b2b38bf01b&#8220; header_font_size=&#8220;35px&#8220; header_2_font=&#8220;&#8211;et_global_heading_font||||||||&#8220; header_2_text_color=&#8220;gcid-f5853230-0d63-4130-b142-81b2b38bf01b&#8220; global_colors_info=&#8220;{%22gcid-f5853230-0d63-4130-b142-81b2b38bf01b%22:%91%22header_2_text_color%22,%22header_text_color%22%93}&#8220;]<\/p>\n<h1 class=\"p1\"><span class=\"s1\"><b>Gletscherm\u00fchlen und Gletschert\u00f6pfe<\/b><\/span><\/h1>\n<p>&nbsp;<\/p>\n<h3 class=\"p1\"><span class=\"s1\"><b>Die verborgenen Tunnel des Wassers<\/b><\/span><\/h3>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8220;2_5&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8220;3_5,2_5&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; width=&#8220;100%&#8220; custom_padding=&#8220;0px|20px|0%|20px|false|false&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_column type=&#8220;3_5&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_text _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; text_text_color=&#8220;gcid-f5853230-0d63-4130-b142-81b2b38bf01b&#8220; header_4_font=&#8220;|700|||||||&#8220; header_4_text_color=&#8220;gcid-f5853230-0d63-4130-b142-81b2b38bf01b&#8220; custom_padding=&#8220;|5%|||false|false&#8220; global_colors_info=&#8220;{%22gcid-f5853230-0d63-4130-b142-81b2b38bf01b%22:%91%22text_text_color%22,%22header_4_text_color%22%93}&#8220;]<\/p>\n<p class=\"p1\"><span class=\"s1\">Wenn Schmelzwasser durch Spalten in die Oberfl\u00e4che eines Gletschers eindringt, beginnt ein spektakul\u00e4rer Prozess. Das Wasser, oft beladen mit Sand und Steinen , frisst sich wie ein Bohrer in die Tiefe und schafft Gletscherm\u00fchlen: senkrechte Sch\u00e4chte, die bis zu 20 Meter Durchmesser und mehrere hundert Meter Tiefe erreichen k\u00f6nnen. Die rotierende Bewegung des Wassers erzeugt spiralf\u00f6rmige und verschlungene Hohlr\u00e4ume, die das Eis von innen heraus formen.<\/span><\/p>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8220;2_5&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_heading title=&#8220;2&#8243; _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; title_text_align=&#8220;right&#8220; title_text_color=&#8220;gcid-1d0ad49c-260c-4939-ba6c-ca42425f0a60&#8243; title_font_size=&#8220;36vw&#8220; transform_translate_linked=&#8220;off&#8220; z_index=&#8220;20&#8243; custom_margin=&#8220;-40%|0px|-78%||false|false&#8220; custom_margin_tablet=&#8220;-10%|9%|-22%||false|false&#8220; custom_margin_phone=&#8220;-6%||-27%||false|false&#8220; custom_margin_last_edited=&#8220;on|tablet&#8220; title_font_size_tablet=&#8220;41vw&#8220; title_font_size_phone=&#8220;60vw&#8220; title_font_size_last_edited=&#8220;on|desktop&#8220; global_colors_info=&#8220;{%22gcid-1d0ad49c-260c-4939-ba6c-ca42425f0a60%22:%91%22title_text_color%22%93}&#8220;][\/et_pb_heading][\/et_pb_column][\/et_pb_row][et_pb_row module_class=&#8220;immagine-stazione&#8220; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; z_index=&#8220;0&#8243; width=&#8220;100%&#8220; custom_padding=&#8220;|20px||20px|false|true&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_column type=&#8220;4_4&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_image title_text=&#8220;Icefields Parkway&#8220; _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; background_image=&#8220;https:\/\/icewalk.it\/wp-content\/uploads\/2025\/10\/Bild-02a-Athabasca.Moulin.jpg&#8220; parallax=&#8220;on&#8220; custom_margin_tablet=&#8220;&#8220; custom_margin_phone=&#8220;-80px||||false|false&#8220; custom_margin_last_edited=&#8220;on|phone&#8220; custom_padding=&#8220;50%||||false|false&#8220; custom_padding_tablet=&#8220;50%||||false|false&#8220; custom_padding_phone=&#8220;100%||||false|false&#8220; custom_padding_last_edited=&#8220;on|phone&#8220; global_colors_info=&#8220;{}&#8220;][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8220;1_2,1_2&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; width=&#8220;100%&#8220; custom_padding=&#8220;|20px|54px|20px|false|false&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_column type=&#8220;1_2&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_text _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; text_text_color=&#8220;gcid-f5853230-0d63-4130-b142-81b2b38bf01b&#8220; header_4_font=&#8220;|700|||||||&#8220; header_4_text_color=&#8220;gcid-f5853230-0d63-4130-b142-81b2b38bf01b&#8220; custom_padding=&#8220;|5%|||false|false&#8220; global_colors_info=&#8220;{%22gcid-f5853230-0d63-4130-b142-81b2b38bf01b%22:%91%22text_text_color%22,%22header_4_text_color%22%93}&#8220;]<\/p>\n<p class=\"p1\"><span class=\"s1\">Diese Strukturen sind entscheidend f\u00fcr das innere Wassersystem des Gletschers. Sie beschleunigen den Abfluss des Schmelzwassers und beeinflussen, wie schnell sich der Gletscher \u00fcber sein Felsbett bewegt. Stauen sich gro\u00dfe Wassermengen in den Gletscherm\u00fchlen, steigt der Druck in den Reservoiren an der Basis stark an. Bricht ein solcher Speicher auf, entstr\u00f6mt das Wasser unter hohem Druck \u2013 bei einer 100 m hohen Wassers\u00e4ule entspricht das 10 bar \u2013 und mit hoher Geschwindigkeit.<\/span><\/p>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8220;1_2&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; width_tablet=&#8220;100%&#8220; width_phone=&#8220;100%&#8220; width_last_edited=&#8220;on|tablet&#8220; custom_padding=&#8220;2px|20px|66px|20px|false|false&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_column type=&#8220;4_4&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_image src=&#8220;https:\/\/icewalk.it\/wp-content\/uploads\/2025\/10\/grafici31_de.jpg&#8220; title_text=&#8220;grafici31_de&#8220; _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; background_enable_image=&#8220;off&#8220; custom_padding=&#8220;|||0px|false|false&#8220; global_colors_info=&#8220;{}&#8220;][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8220;1_2,1_2&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; width=&#8220;100%&#8220; custom_padding=&#8220;|20px|0px|20px|false|false&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_column type=&#8220;1_2&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_text _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; text_text_color=&#8220;gcid-f5853230-0d63-4130-b142-81b2b38bf01b&#8220; header_4_font=&#8220;|700|||||||&#8220; header_4_text_color=&#8220;gcid-f5853230-0d63-4130-b142-81b2b38bf01b&#8220; custom_padding=&#8220;|5%|||false|false&#8220; global_colors_info=&#8220;{%22gcid-f5853230-0d63-4130-b142-81b2b38bf01b%22:%91%22text_text_color%22,%22header_4_text_color%22%93}&#8220;]<\/p>\n<h3 class=\"p1\"><span class=\"s1\">Trifft das Wasser schlie\u00dflich auf den Fels, entstehen <b><i>Gletschert\u00f6pfe<\/i><\/b>: zylindrische oder sch\u00fcsself\u00f6rmige Vertiefungen, die durch Wirbelstr\u00f6mungen im Schmelzwasser geformt werden. In diesen Strudeln k\u00f6nnen Flie\u00dfgeschwindigkeiten von bis zu 200 km\/h erreicht werden , wobei Sand und Ger\u00f6ll die Gesteinsoberfl\u00e4che aush\u00f6hlen. Solche Formen sind meist mehrere Zentimeter bis Meter gro\u00df und stammen h\u00e4ufig aus der letzten Eiszeit.<\/span><\/h3>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8220;1_2&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_image src=&#8220;https:\/\/icewalk.it\/wp-content\/uploads\/2025\/10\/Bild-05-DSC01254-e1759833501913.jpg&#8220; title_text=&#8220;Bild 05 DSC01254&#8243; _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8220;1_2,1_2&#8243; custom_padding_last_edited=&#8220;on|desktop&#8220; _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; width=&#8220;100%&#8220; custom_padding=&#8220;38px|20px|33px|20px|false|false&#8220; custom_padding_tablet=&#8220;38px|20px|80px|20px|false|false&#8220; custom_padding_phone=&#8220;20px||20px||false|false&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_column type=&#8220;1_2&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][\/et_pb_column][et_pb_column type=&#8220;1_2&#8243; _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_text _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; text_text_color=&#8220;gcid-f5853230-0d63-4130-b142-81b2b38bf01b&#8220; header_4_font=&#8220;|700|||||||&#8220; header_4_text_color=&#8220;gcid-f5853230-0d63-4130-b142-81b2b38bf01b&#8220; custom_padding=&#8220;|5%|||false|false&#8220; global_colors_info=&#8220;{%22gcid-f5853230-0d63-4130-b142-81b2b38bf01b%22:%91%22text_text_color%22,%22header_4_text_color%22%93}&#8220;]<\/p>\n<p class=\"p1\"><span class=\"s1\">Die \u00e4ltere Vorstellung, dass gro\u00dfe Bl\u00f6cke im Eis diese L\u00f6cher durch st\u00e4ndige Drehbewegungen \u201emahlen\u201c, gilt heute als \u00fcberholt. Es ist die Kraft des Wassers \u2013 Druck, Rotation und mitgef\u00fchrte Sedimente \u2013, die diese eindrucksvollen Naturformen hervorbringt.<\/span><\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8220;2_3,1_3&#8243; custom_padding_last_edited=&#8220;on|desktop&#8220; _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; width_tablet=&#8220;100%&#8220; width_phone=&#8220;100%&#8220; width_last_edited=&#8220;on|tablet&#8220; custom_padding=&#8220;68px|20px|0px|20px|false|false&#8220; custom_padding_tablet=&#8220;68px|20px|50px|20px|false|false&#8220; custom_padding_phone=&#8220;0px|20px|30px|20px|false|false&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_column type=&#8220;2_3&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_image src=&#8220;https:\/\/icewalk.it\/wp-content\/uploads\/2026\/01\/DJI_0154.jpg&#8220; title_text=&#8220;DCIM101MEDIADJI_0154.JPG&#8220; 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title_text=&#8220;Bild 04a Unter dem Gletscher VM1&#8243; _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; background_enable_image=&#8220;off&#8220; custom_margin=&#8220;||13px|||&#8220; custom_padding=&#8220;||||false|false&#8220; global_colors_info=&#8220;{}&#8220;][\/et_pb_image][et_pb_text _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;]<\/p>\n<p>Gletschertor<\/p>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8220;2_5&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_image src=&#8220;https:\/\/icewalk.it\/wp-content\/uploads\/2025\/10\/Bild-04c-Unter-dem-Gletscher_VM.jpg&#8220; title_text=&#8220;Bild 04c Unter dem Gletscher_VM&#8220; _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; background_enable_image=&#8220;off&#8220; custom_padding=&#8220;||||false|false&#8220; global_colors_info=&#8220;{}&#8220;][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; width_tablet=&#8220;&#8220; width_phone=&#8220;90%&#8220; width_last_edited=&#8220;on|phone&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_column type=&#8220;4_4&#8243; _builder_version=&#8220;4.27.3&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_image src=&#8220;https:\/\/icewalk.it\/wp-content\/uploads\/2025\/10\/grafici28_de.jpg&#8220; title_text=&#8220;grafici28_de&#8220; _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; background_enable_image=&#8220;off&#8220; custom_margin=&#8220;||61px|||&#8220; custom_padding=&#8220;||||false|false&#8220; global_colors_info=&#8220;{}&#8220;][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_column type=&#8220;4_4&#8243; _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; global_colors_info=&#8220;{}&#8220;][et_pb_text _builder_version=&#8220;4.27.4&#8243; _module_preset=&#8220;default&#8220; text_font_size=&#8220;50px&#8220; text_orientation=&#8220;center&#8220; width=&#8220;100%&#8220; max_width=&#8220;100%&#8220; custom_margin=&#8220;|0px||0px|false|false&#8220; custom_padding=&#8220;|0px||0px|false|false&#8220; custom_padding_tablet=&#8220;&#8220; custom_padding_phone=&#8220;|5%||5%|false|false&#8220; custom_padding_last_edited=&#8220;on|phone&#8220; global_colors_info=&#8220;{}&#8220;]<\/p>\n<p class=\"p1\" style=\"text-align: center;\"><nav class=\"nine-steps-nav fullprogress\" role=\"navigation\" aria-label=\"Navigazione capitoli\" style=\"--step:0\"><a href=\"https:\/\/icewalk.it\/de\/erosion\/\" aria-label=\"Capitolo 1\" class=\"\">1<\/a><a href=\"https:\/\/icewalk.it\/de\/gletschertoepfe\/\" aria-label=\"Capitolo 2\" class=\"\">2<\/a><a href=\"https:\/\/icewalk.it\/de\/rundhoecker\/\" aria-label=\"Capitolo 3\" class=\"\">3<\/a><\/nav><\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Gletscherm\u00fchlen und Gletschert\u00f6pfe &nbsp; Die verborgenen Tunnel des WassersWenn Schmelzwasser durch Spalten in die Oberfl\u00e4che eines Gletschers eindringt, beginnt ein spektakul\u00e4rer Prozess. Das Wasser, oft beladen mit Sand und Steinen , frisst sich wie ein Bohrer in die Tiefe und schafft Gletscherm\u00fchlen: senkrechte Sch\u00e4chte, die bis zu 20 Meter Durchmesser und mehrere hundert Meter Tiefe [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"open","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":""},"class_list":["post-1285","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/icewalk.it\/de\/wp-json\/wp\/v2\/pages\/1285","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/icewalk.it\/de\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/icewalk.it\/de\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/icewalk.it\/de\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/icewalk.it\/de\/wp-json\/wp\/v2\/comments?post=1285"}],"version-history":[{"count":0,"href":"https:\/\/icewalk.it\/de\/wp-json\/wp\/v2\/pages\/1285\/revisions"}],"wp:attachment":[{"href":"https:\/\/icewalk.it\/de\/wp-json\/wp\/v2\/media?parent=1285"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}