{"id":282,"date":"2025-11-21T18:24:23","date_gmt":"2025-11-21T17:24:23","guid":{"rendered":"https:\/\/mostre.cnr.it\/antartide\/?p=282"},"modified":"2025-11-29T18:06:27","modified_gmt":"2025-11-29T17:06:27","slug":"la-geografia-dellantartide","status":"publish","type":"post","link":"https:\/\/mostre.cnr.it\/antartide\/la-geografia-dellantartide\/","title":{"rendered":"La geografia dell\u2019Antartide"},"content":{"rendered":"

[et_pb_section fb_built=”1″ fullwidth=”on” admin_label=”Section” _builder_version=”4.27.4″ custom_margin_tablet=”” custom_margin_phone=”-5px||||false|false” custom_margin_last_edited=”on|phone” bottom_divider_style=”mountains2″ bottom_divider_color=”#FFFFFF” global_colors_info=”{}”][et_pb_fullwidth_image title_text=”lake-fryxell-in-the-transantarctic-mountains-antarctica_800x600″ admin_label=”Fullwidth Image” _builder_version=”4.27.4″ vertical_offset=”-187px” max_height=”300px” overflow-y=”visible” custom_margin=”0px||0px||false|false” custom_padding=”||0px||false|false” animation_style=”fade” animation_duration=”500ms” animation=”fade_in” use_border_color=”off” border_color=”#ffffff” border_style=”solid” global_colors_info=”{}”][\/et_pb_fullwidth_image][et_pb_fullwidth_header title=”La geografia dell\u2019Antartide” text_orientation=”center” button_one_text=”scarica il pannello” button_one_url=”https:\/\/mostre.cnr.it\/antartide\/wp-content\/uploads\/sites\/4\/2025\/11\/Pannello_Antartide-1_low.pdf” _builder_version=”4.27.4″ _module_preset=”default” title_font=”Urbanist|600|||||||” title_text_align=”center” title_font_size=”55px” title_line_height=”1.3em” background_color=”#88C4DD” custom_button_one=”on” custom_margin=”-5px||||false|false” custom_margin_tablet=”-6px|||||” custom_margin_phone=”0px|||0px|false|false” custom_margin_last_edited=”on|phone” custom_padding=”0px|||0px|false|false” link_option_url_new_window=”on” title_font_tablet=”Urbanist|600|||||||” title_font_phone=”Urbanist|600|||||||” title_font_last_edited=”on|phone” title_font_size_tablet=”55px” title_font_size_phone=”38px” title_font_size_last_edited=”on|phone” title_letter_spacing_tablet=”” title_letter_spacing_phone=”0px” title_letter_spacing_last_edited=”on|phone” button_one_text_size_tablet=”” button_one_text_size_phone=”16px” button_one_text_size_last_edited=”on|phone” global_colors_info=”{}”][\/et_pb_fullwidth_header][\/et_pb_section][et_pb_section fb_built=”1″ specialty=”on” _builder_version=”4.27.4″ _module_preset=”default” top_divider_height_tablet=”” top_divider_height_phone=”” top_divider_height_last_edited=”on|phone” global_colors_info=”{}”][et_pb_column type=”1_2″ specialty_columns=”2″ _builder_version=”4.16″ custom_padding=”|||” global_colors_info=”{}” custom_padding__hover=”|||”][et_pb_row_inner _builder_version=”4.27.4″ _module_preset=”default” custom_margin_tablet=”” custom_margin_phone=”||0px||false|false” custom_margin_last_edited=”on|phone” custom_padding=”||0px||false|false” global_colors_info=”{}”][et_pb_column_inner saved_specialty_column_type=”1_2″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text admin_label=”Text” _builder_version=”4.27.4″ text_font=”Inter|300|||||||” text_text_color=”#303030″ text_font_size=”16px” text_line_height=”1.6em” background_size=”initial” background_position=”top_left” background_repeat=”repeat” max_width_tablet=”” max_width_phone=”” max_width_last_edited=”on|desktop” custom_margin_tablet=”” custom_margin_phone=”-50px||||false|false” custom_margin_last_edited=”on|phone” text_font_tablet=”Inter|300|||||||” text_font_phone=”Inter|300|||||||” text_font_last_edited=”on|phone” use_border_color=”off” border_color=”#ffffff” border_style=”solid” global_colors_info=”{}”]<\/p>\n

L\u2019Antartide \u00e8 il continente pi\u00f9 remoto e inospitale della Terra, ma anche uno dei pi\u00f9 affascinanti. Di forma quasi circolare, con le due ampie insenature del Mare di Ross e del Mare di Weddell ricoperte da estese piattaforme di ghiaccio, l\u2019Antartide \u00e8 per estensione il quinto dei sette continenti<\/strong>. Durante l’estate australe, l\u2019Antartide ha una superficie di 14 milioni di chilometri quadrati: pari a circa 45 volte quella dell\u2019Italia. In inverno la superficie raddoppia a causa della formazione di una estesa banchisa che circonda il continente.<\/span><\/p>\n

Oltre il 98% del continente \u00e8 coperto da una coltre glaciale che costituisce circa il 90% del ghiaccio terrestre e il 70% dell\u2019acqua dolce del pianeta<\/strong>. La presenza della spessa calotta glaciale fa dell\u2019Antartide il continente con l\u2019altitudine media pi\u00f9 elevata: circa 2.300 metri.<\/span><\/p>\n

[\/et_pb_text][et_pb_image src=”https:\/\/mostre.cnr.it\/antartide\/wp-content\/uploads\/sites\/4\/2025\/11\/transantarctic-mountains-antarctica_800x600.jpg” title_text=”transantarctic-mountains-antarctica_800x600″ align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” disabled_on=”on|off|off” admin_label=”Image” _builder_version=”4.27.4″ custom_margin=”80px|||||” animation_style=”fade” animation_duration=”500ms” border_radii=”on|30px|30px|30px|30px” animation=”fade_in” use_border_color=”off” border_color=”#ffffff” border_style=”solid” sticky=”off” always_center_on_mobile=”on” global_colors_info=”{}”][\/et_pb_image][et_pb_gallery gallery_ids=”25283,25282,25281″ fullwidth=”on” disabled_on=”off|on|on” _builder_version=”4.27.4″ _module_preset=”default” custom_margin_tablet=”” custom_margin_phone=”” custom_margin_last_edited=”on|phone” border_radii=”on|20px|20px|20px|20px” global_colors_info=”{}”][\/et_pb_gallery][\/et_pb_column_inner][\/et_pb_row_inner][\/et_pb_column][et_pb_column type=”1_2″ _builder_version=”4.16″ custom_padding=”|||” global_colors_info=”{}” custom_padding__hover=”|||”][et_pb_image src=”https:\/\/mostre.cnr.it\/antartide\/wp-content\/uploads\/sites\/4\/2025\/11\/antarctica-map800x600.jpg” title_text=”antarctica-map800x600_credits:https:\/\/mapswire.com\/” show_in_lightbox=”on” align=”right” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” disabled_on=”on|off|off” admin_label=”Image” _builder_version=”4.27.4″ custom_margin=”||45px|||” custom_padding=”0px||||false|false” animation_style=”fade” animation_duration=”500ms” border_radii=”on|30px|30px|30px|30px” animation=”fade_in” use_border_color=”off” border_color=”#ffffff” border_style=”solid” sticky=”off” always_center_on_mobile=”on” global_colors_info=”{}”][\/et_pb_image][et_pb_text admin_label=”Text” _builder_version=”4.27.4″ text_font=”Inter|300|||||||” text_text_color=”#303030″ text_font_size=”16px” text_line_height=”1.6em” background_size=”initial” background_position=”top_left” background_repeat=”repeat” width_tablet=”” width_phone=”” width_last_edited=”on|phone” max_width_tablet=”” max_width_phone=”” max_width_last_edited=”on|desktop” custom_margin_tablet=”10%||10%|10%” custom_margin_phone=”5%||5%|0%|false|false” custom_margin_last_edited=”on|desktop” custom_padding=”0px|||||” use_border_color=”off” border_color=”#ffffff” border_style=”solid” global_colors_info=”{}”]<\/p>\n

Il continente \u00e8 formato da due regioni principali: l\u2019Antartide orientale, pi\u00f9 estesa, e quella occidentale, che include la Penisola Antartica.<\/p>\n

Le due aree sono separate dalla catena delle Montagne Transantartiche<\/strong>, in gran parte sepolta sotto il ghiaccio. Il margine occidentale di questa lunga catena rappresenta attualmente una zona di distensione lungo la quale sono localizzati alcuni vulcani recenti e attivi.<\/p>\n

Senza la calotta glaciale, l\u2019Antartide rivelerebbe una geografia complessa, fatta di catene montuose, valli, pianure, mari interni e isole. La parte occidentale apparirebbe come un arcipelago.<\/p>\n

Il ghiaccio della calotta antartica \u00e8 in costante movimento: giganteschi ghiacciai scorrono lentamente verso le coste, solcati da profondi crepacci. Giunti al mare formano imponenti piattaforme di ghiaccio, tra cui la Piattaforma di Ross, grande quanto la Francia. Quando i margini di queste piattaforme si fratturano, si staccano enormi iceberg tabulari che si disperdono nell\u2019oceano.<\/span><\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_section][et_pb_section fb_built=”1″ specialty=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#D2E4F9″ global_colors_info=”{}”][et_pb_column type=”1_2″ specialty_columns=”2″ _builder_version=”4.16″ custom_padding=”|||” global_colors_info=”{}” custom_padding__hover=”|||”][et_pb_row_inner _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_column_inner saved_specialty_column_type=”1_2″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text admin_label=”Text” _builder_version=”4.27.4″ text_font=”Urbanist||||||||” text_text_color=”#303030″ text_font_size=”45px” text_line_height=”1.1em” background_size=”initial” background_position=”top_left” background_repeat=”repeat” max_width_tablet=”” max_width_phone=”” max_width_last_edited=”on|desktop” custom_margin=”||15px||false|false” custom_margin_tablet=”10%||10%|10%” custom_margin_phone=”-10%||10%|0%|false|false” custom_margin_last_edited=”on|desktop” text_text_color_tablet=”#303030″ text_text_color_phone=”#303030″ text_text_color_last_edited=”on|phone” text_font_size_tablet=”45px” text_font_size_phone=”35px” text_font_size_last_edited=”on|phone” use_border_color=”off” border_color=”#ffffff” border_style=”solid” global_colors_info=”{}”]<\/p>\n

Idrografia subglaciale: laghi nascosti e vita estrema<\/p>\n

[\/et_pb_text][et_pb_text admin_label=”Text” _builder_version=”4.27.4″ text_font=”Inter|300|||||||” text_text_color=”#303030″ text_font_size=”16px” text_line_height=”1.6em” background_size=”initial” background_position=”top_left” background_repeat=”repeat” max_width_tablet=”” max_width_phone=”” max_width_last_edited=”on|desktop” use_border_color=”off” border_color=”#ffffff” border_style=”solid” global_colors_info=”{}”]Alla base della calotta glaciale, a profondit\u00e0 superiori ai 2.500 metri, l\u2019elevata pressione pu\u00f2 far fondere il ghiaccio anche sotto zero gradi centigradi. L\u2019acqua che ne deriva si concentra in un complesso sistema idrografico subglaciale costituito da un sistema di laghi, fiumi e canali, spesso collegati tra loro. Questa rete idrica pu\u00f2 facilitare lo scorrimento del ghiaccio sovrastante, agendo da \u2018cuscinetto\u2019 e influenzando i movimenti della calotta. <\/p>\n

I laghi subglaciali costituiscono ecosistemi con caratteristiche uniche sulla Terra quali: pressioni sino a 400 volte superiori a quelle atmosferiche, temperature intorno a 2-3 gradi al di sotto di 0\u00b0C, assenza di luce. Recentemente, nelle acque dei laghi subglaciali sono state trovate forme di vita primitiva, tra cui alcuni batteri, virus e altri organismi unicellulari fino ad ora sconosciuti.[\/et_pb_text][\/et_pb_column_inner][\/et_pb_row_inner][\/et_pb_column][et_pb_column type=”1_2″ _builder_version=”4.16″ custom_padding=”|||” global_colors_info=”{}” custom_padding__hover=”|||”][et_pb_video src=”https:\/\/mostre.cnr.it\/wp-content\/uploads\/sites\/4\/2025\/11\/HDplumb_1280x720_5994_1080p59.94.mp4″ play_icon_color=”#FFFFFF” font_icon=”||fa||900″ _builder_version=”4.27.4″ _module_preset=”default” custom_margin=”||-2px|||” border_radii=”on|25px|25px|25px|25px” global_colors_info=”{}”][\/et_pb_video][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” text_font=”Inter|300|||||||” text_text_color=”#00208A” text_line_height=”1.5em” custom_padding=”15px||||false|false” global_colors_info=”{}”]<\/p>\n

Questa animazione illustra le dinamiche della rete di laghi subglaciali situati molto al di sotto dei flussi di ghiaccio dell’Antartide – @NASA\/Goddard Space Flight Center Conceptual Image Lab<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_section][et_pb_section fb_built=”1″ specialty=”on” _builder_version=”4.27.4″ _module_preset=”default” background_enable_color=”off” global_colors_info=”{}”][et_pb_column type=”1_2″ specialty_columns=”2″ _builder_version=”4.16″ custom_padding=”|||” global_colors_info=”{}” custom_padding__hover=”|||”][et_pb_row_inner _builder_version=”4.27.4″ _module_preset=”default” custom_margin_tablet=”” custom_margin_phone=”0px||0px||false|false” custom_margin_last_edited=”on|phone” custom_padding=”0px||0px||false|false” global_colors_info=”{}”][et_pb_column_inner saved_specialty_column_type=”1_2″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text admin_label=”Text” _builder_version=”4.27.4″ text_font=”Urbanist||||||||” text_text_color=”#303030″ text_font_size=”45px” text_line_height=”1.1em” background_size=”initial” background_position=”top_left” background_repeat=”repeat” max_width_tablet=”” max_width_phone=”” max_width_last_edited=”on|desktop” custom_margin=”||15px||false|false” custom_margin_tablet=”10%||10%|10%” custom_margin_phone=”0%||5%|0%|false|false” custom_margin_last_edited=”on|desktop” text_font_size_tablet=”45px” text_font_size_phone=”35px” text_font_size_last_edited=”on|phone” use_border_color=”off” border_color=”#ffffff” border_style=”solid” global_colors_info=”{}”]<\/p>\n

Un confine invisibile: la Convergenza Antartica<\/span><\/p>\n

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Il vero confine dell\u2019ambiente antartico si estende oltre la massa continentale e comprende le acque fino alla cosiddetta \u201cConvergenza Antartica\u201d. Si tratta di un\u2019ampia fascia di oceano larga circa 40 km<\/strong>, percorsa in senso orario da una intensa corrente marina che separa le acque fredde dell\u2019Antartide da quelle pi\u00f9 calde subantartiche<\/strong>.<\/p>\n

Le differenze di temperatura, salinit\u00e0 e densit\u00e0 creano una barriera quasi fisica fra l\u2019Oceano Meridionale e gli altri oceani.
La Convergenza Antartica esiste da circa 20 milioni di anni. Durante questo periodo ci sono stati pochi scambi di vita marina da un lato all\u2019altro. Ci\u00f2 rende l\u2019Antartide un\u2019area geografica unica<\/strong> per gli studi sull\u2019evoluzione e l\u2019adattamento degli organismi.<\/p>\n

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L\u2019Antartide in cifre<\/p>\n

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Superficie totale<\/span><\/p>\n

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Volume dei ghiacci<\/span><\/p>\n

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Altitudine media<\/span><\/p>\n

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Altitudine del Polo Sud<\/span><\/p>\n

[\/et_pb_blurb][\/et_pb_column][et_pb_column type=”1_6″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_blurb title=”-89.2\u00b0C” image=”https:\/\/mostre.cnr.it\/antartide\/wp-content\/uploads\/sites\/4\/2025\/11\/temperature.svg” image_icon_width=”60%” _builder_version=”4.27.4″ _module_preset=”default” header_font=”Montserrat|700|||||||” header_text_color=”#0C71C3″ header_font_size=”19px” body_font=”Inter||||||||” body_font_size=”15px” body_line_height=”1.3em” text_orientation=”center” global_colors_info=”{}”]<\/p>\n

Temperatura minima registrata (Stazione Vostok luglio 1983)<\/span><\/p>\n

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Velocit\u00e0 massima del vento misurata (Dumont D\u2019Urville, luglio 1972)<\/span><\/p>\n

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Accumulo nevoso annuo<\/span><\/p>\n

[\/et_pb_blurb][\/et_pb_column][et_pb_column type=”1_6″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_blurb title=”4.776 m” image=”https:\/\/mostre.cnr.it\/antartide\/wp-content\/uploads\/sites\/4\/2025\/11\/spessore-ghiaccio2.svg” image_icon_width=”60%” _builder_version=”4.27.4″ _module_preset=”default” header_font=”Montserrat|700|||||||” header_text_color=”#0C71C3″ header_font_size=”19px” body_font=”Inter||||||||” body_font_size=”15px” body_line_height=”1.3em” text_orientation=”center” global_colors_info=”{}”]<\/p>\n

Il massimo spessore dei ghiacci (nella Terra Ad\u00e9lie)<\/span><\/p>\n

[\/et_pb_blurb][\/et_pb_column][et_pb_column type=”1_6″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_blurb title=”31.000 km\u00b2” image=”https:\/\/mostre.cnr.it\/antartide\/wp-content\/uploads\/sites\/4\/2025\/11\/iceberg-1.svg” image_icon_width=”60%” _builder_version=”4.27.4″ _module_preset=”default” header_font=”Montserrat|700|||||||” header_text_color=”#0C71C3″ header_font_size=”19px” body_font=”Inter||||||||” body_font_size=”15px” body_line_height=”1.3em” text_orientation=”center” global_colors_info=”{}”]<\/p>\n

Il pi\u00f9 grande iceberg osservato nel 1956 (pi\u00f9 esteso del Belgio)<\/span><\/p>\n

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Lago subglaciale pi\u00f9 grande: Vostok, profondit\u00e0 900 m<\/span><\/p>\n

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La massima depressione: Bacino subglaciale Bentley<\/span><\/p>\n

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La cima pi\u00f9 elevata Monte Vinson<\/span><\/p>\n

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L\u2019Antartide in cifre<\/p>\n

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Superficie totale<\/span><\/p>\n

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Altitudine media<\/span><\/p>\n

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Velocit\u00e0 massima del vento misurata (Dumont D\u2019Urville, luglio 1972)<\/span><\/p>\n

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Volume dei ghiacci<\/span><\/p>\n

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Altitudine del Polo Sud<\/span><\/p>\n

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Temperatura minima registrata (Stazione Vostok luglio 1983)<\/span><\/p>\n

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Accumulo nevoso annuo<\/span><\/p>\n

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Lago subglaciale pi\u00f9 grande: Vostok, profondit\u00e0 900 m<\/span><\/p>\n

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La cima pi\u00f9 elevata Monte Vinson<\/span><\/p>\n

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Il massimo spessore dei ghiacci (nella Terra Ad\u00e9lie)<\/span><\/p>\n

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Il pi\u00f9 grande iceberg osservato nel 1956 (pi\u00f9 esteso del Belgio)<\/span><\/p>\n

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La massima depressione: Bacino subglaciale Bentley<\/span><\/p>\n

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L\u2019Antartide \u00e8 il continente pi\u00f9 remoto e inospitale della Terra, ma anche uno dei pi\u00f9 affascinanti. Di forma quasi circolare, con le due ampie insenature del Mare di Ross e del Mare di Weddell ricoperte da estese piattaforme di ghiaccio, l\u2019Antartide \u00e8 per estensione il quinto dei sette continenti. Durante l’estate australe, l\u2019Antartide ha una […]<\/p>\n","protected":false},"author":1,"featured_media":193,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"2880","footnotes":""},"categories":[1],"tags":[],"dipi_cpt_category":[],"class_list":["post-282","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-senza-categoria"],"_links":{"self":[{"href":"https:\/\/mostre.cnr.it\/antartide\/wp-json\/wp\/v2\/posts\/282","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/mostre.cnr.it\/antartide\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/mostre.cnr.it\/antartide\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/mostre.cnr.it\/antartide\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/mostre.cnr.it\/antartide\/wp-json\/wp\/v2\/comments?post=282"}],"version-history":[{"count":59,"href":"https:\/\/mostre.cnr.it\/antartide\/wp-json\/wp\/v2\/posts\/282\/revisions"}],"predecessor-version":[{"id":25635,"href":"https:\/\/mostre.cnr.it\/antartide\/wp-json\/wp\/v2\/posts\/282\/revisions\/25635"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/mostre.cnr.it\/antartide\/wp-json\/wp\/v2\/media\/193"}],"wp:attachment":[{"href":"https:\/\/mostre.cnr.it\/antartide\/wp-json\/wp\/v2\/media?parent=282"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/mostre.cnr.it\/antartide\/wp-json\/wp\/v2\/categories?post=282"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/mostre.cnr.it\/antartide\/wp-json\/wp\/v2\/tags?post=282"},{"taxonomy":"dipi_cpt_category","embeddable":true,"href":"https:\/\/mostre.cnr.it\/antartide\/wp-json\/wp\/v2\/dipi_cpt_category?post=282"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}