Liv Glacier is a steep valley glacier, 64 km (40 mi) long, emerging from the Antarctic Plateau just southeast of Barnum Peak and draining north through the Queen Maud Mountains to enter Ross Ice Shelf between Mayer Crags and Duncan Mountains. It was discovered in 1911 by Roald Amundsen, who named it for the daughter of Fridtjof Nansen. The airway above the Liv Glacier was used by the monoplane Floyd Bennett in 1929 as the route for the first journey to the South Pole by air.
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| - Liv-Gletscher (de)
- Glacier Liv (fr)
- Ghiacciaio Liv (it)
- Liv Glacier (en)
- Liv Glacier (sv)
- 利夫冰川 (zh)
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| - Der Liv-Gletscher ist ein steiler, rund 65 km langer Talgletscher in der antarktischen Ross Dependency. Er fließt vom Polarplateau südöstlich des Barnum Peak in nördlicher Richtung durch das Königin-Maud-Gebirge zum Ross-Schelfeis, das er zwischen den Mayer Crags und den Duncan Mountains an der Dufek-Küste erreicht. Der norwegische Polarforscher Roald Amundsen entdeckte ihn 1911 beim Marsch zum geographischen Südpol im Rahmen seiner Antarktisexpedition (1910–1912). Er benannte ihn nach Liv Nansen (1893–1959), der ältesten Tochter des norwegischen Polarforschers Fridtjof Nansen. (de)
- Le glacier Liv est un glacier entre la chaîne du Prince-Olav à l'ouest et la chaîne Duncan et le chaînon Herbert à l'est, dans la chaîne de la Reine-Maud, en Antarctique. Il est découvert en 1911 par Roald Amundsen, qui le nomme en l'honneur de la fille de Fridtjof Nansen. (fr)
- Liv Glacier är en glaciär i Antarktis. Den ligger i Västantarktis. Nya Zeeland gör anspråk på området. Liv Glacier ligger 250 meter över havet. Terrängen runt Liv Glacier är varierad. Den högsta punkten i närheten är 1 033 meter över havet, 4,7 kilometer väster om Liv Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten. (sv)
- 利夫冰川（英語：Liv Glacier）是南極洲的冰川，全長64公里，發源地在南極高原的巴納姆峰東南面，最終注入羅斯冰架，該冰川在1911年11月由挪威極地探險家羅爾德·阿蒙森發現。 (zh)
- Liv Glacier is a steep valley glacier, 64 km (40 mi) long, emerging from the Antarctic Plateau just southeast of Barnum Peak and draining north through the Queen Maud Mountains to enter Ross Ice Shelf between Mayer Crags and Duncan Mountains. It was discovered in 1911 by Roald Amundsen, who named it for the daughter of Fridtjof Nansen. The airway above the Liv Glacier was used by the monoplane Floyd Bennett in 1929 as the route for the first journey to the South Pole by air. (en)
- Il Ghiacciaio Liv (in lingua inglese: Liv Glacier) è un ripido ghiacciaio vallivo antartico, lungo 64 km che si origina dall'Altopiano Antartico appena a sudest del Barnum Peak, fluendo in direzione nord attraverso i Monti della Regina Maud, in Antartide. Termina il suo percorso andando a entrare nella Barriera di Ross, tra i Mayer Crags e le Duncan Mountains. Fu scoperto nel 1911 dall'esploratore norvegese Roald Amundsen, che ne assegnò la denominazione in onore di Liv Nansen (1893–1959), la figlia primogenita dell'esploratore Fridtjof Nansen. (it)
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| - Der Liv-Gletscher ist ein steiler, rund 65 km langer Talgletscher in der antarktischen Ross Dependency. Er fließt vom Polarplateau südöstlich des Barnum Peak in nördlicher Richtung durch das Königin-Maud-Gebirge zum Ross-Schelfeis, das er zwischen den Mayer Crags und den Duncan Mountains an der Dufek-Küste erreicht. Der norwegische Polarforscher Roald Amundsen entdeckte ihn 1911 beim Marsch zum geographischen Südpol im Rahmen seiner Antarktisexpedition (1910–1912). Er benannte ihn nach Liv Nansen (1893–1959), der ältesten Tochter des norwegischen Polarforschers Fridtjof Nansen. (de)
- Liv Glacier is a steep valley glacier, 64 km (40 mi) long, emerging from the Antarctic Plateau just southeast of Barnum Peak and draining north through the Queen Maud Mountains to enter Ross Ice Shelf between Mayer Crags and Duncan Mountains. It was discovered in 1911 by Roald Amundsen, who named it for the daughter of Fridtjof Nansen. The airway above the Liv Glacier was used by the monoplane Floyd Bennett in 1929 as the route for the first journey to the South Pole by air. We have investigated the geochemistry of supraglacial streams on the Canada Glacier, Taylor Valley, Antarctica during the 2001–2002 austral summer. Canada Glacier supraglacial streams represent the link between primary precipitation (i.e. glacier snow) and proglacial Lake Hoare. Canada Glacier supraglacial stream geochemistry is intermediate between glacier snow and proglacial stream geochemistry with average concentrations of 49.1 μeq L−1 Ca2+, 19.9 μeq L−1 SO 2−4, and 34.3 μeq L−1 HCO −3. Predominant west to east winds lead to a redistribution of readily soluble salts onto the glacier surface, which is reflected in the geochemistry of the supraglacial streams. Western Canada Glacier supraglacial streams have average SO 2−4:HCO −3 equivalent ratios of 1.0, while eastern supraglacial streams average 0.5, suggesting more sulfate salts reach and dissolve in the western supraglacial streams. A graph of HCO −3 versus Ca2+ for western and eastern supraglacial streams had slopes of 0.87 and 0.72, respectively with R2 values of 0.84 and 0.83. Low concentrations of reactive silicate (> 10 μmol L−1) in the supraglacial streams suggested that little to no silicate weathering occurred on the glacier surface with the exception of cryoconite holes (1000 μmol L−1). Therefore, the major geochemical weathering process occurring in the supraglacial streams is believed to be calcite dissolution. Proglacial stream, Anderson Creek, contains higher concentrations of major ions than supraglacial streams containing 5 times the Ca2+ and 10 times the SO 2−4. Canada Glacier proglacial streams also contain higher concentrations (16.6–30.6 μeq L−1) of reactive silicate than supraglacial streams. This suggests that the controls on glacier meltwater geochemistry switch from calcite and gypsum dissolution to both salt dissolution and silicate mineral weathering as the glacier meltwater evolves. Our chemical mass balance calculations indicate that of the total discharge into Lake Hoare, the final recipient of Canada Glacier meltwater, 81.9% is from direct glacier runoff and 19.1% is from proglacial Andersen Creek. Although during a typical, low melt ablation season Andersen Creek contributes over 40% of the water added to Lake Hoare, its overall chemical importance is diluted by the direct inputs from Canada Glacier during high flow years. Decadal warming events, such as the 2001–2002 austral summer produce supraglacial streams that are a major source of water to Lake Hoare. (en)
- Le glacier Liv est un glacier entre la chaîne du Prince-Olav à l'ouest et la chaîne Duncan et le chaînon Herbert à l'est, dans la chaîne de la Reine-Maud, en Antarctique. Il est découvert en 1911 par Roald Amundsen, qui le nomme en l'honneur de la fille de Fridtjof Nansen. (fr)
- Il Ghiacciaio Liv (in lingua inglese: Liv Glacier) è un ripido ghiacciaio vallivo antartico, lungo 64 km che si origina dall'Altopiano Antartico appena a sudest del Barnum Peak, fluendo in direzione nord attraverso i Monti della Regina Maud, in Antartide. Termina il suo percorso andando a entrare nella Barriera di Ross, tra i Mayer Crags e le Duncan Mountains. Fu scoperto nel 1911 dall'esploratore norvegese Roald Amundsen, che ne assegnò la denominazione in onore di Liv Nansen (1893–1959), la figlia primogenita dell'esploratore Fridtjof Nansen. Il corridoio aereo al di sopra del Ghiacciaio Liv è stato usato nel 1929 dal monoplano Floyd Bennett quale percorso per la prima rotta aerea verso il Polo Sud. (it)
- Liv Glacier är en glaciär i Antarktis. Den ligger i Västantarktis. Nya Zeeland gör anspråk på området. Liv Glacier ligger 250 meter över havet. Terrängen runt Liv Glacier är varierad. Den högsta punkten i närheten är 1 033 meter över havet, 4,7 kilometer väster om Liv Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten. (sv)
- 利夫冰川（英語：Liv Glacier）是南極洲的冰川，全長64公里，發源地在南極高原的巴納姆峰東南面，最終注入羅斯冰架，該冰川在1911年11月由挪威極地探險家羅爾德·阿蒙森發現。 (zh)
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