Horlick Ice Stream (85°17′S 132°00′W / 85.283°S 132.000°W) is a large ice stream on the featureless ice surface to the north of the main mass of the Horlick Mountains of Antarctica, draining west-southwestward, parallel to these mountains, to enter the lower portion of the Reedy Glacier. It was mapped by the U.S. Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names in association with the Horlick Mountains.
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| - Horlick-Eisstrom (de)
- Horlick Ice Stream (en)
- Flusso di ghiaccio Horlick (it)
- 霍利克冰流 (zh)
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| - Horlick Ice Stream (85°17′S 132°00′W / 85.283°S 132.000°W) is a large ice stream on the featureless ice surface to the north of the main mass of the Horlick Mountains of Antarctica, draining west-southwestward, parallel to these mountains, to enter the lower portion of the Reedy Glacier. It was mapped by the U.S. Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names in association with the Horlick Mountains. (en)
- Il flusso di ghiaccio Horlick è un flusso di ghiaccio lungo oltre 100 km situato in Antartide, dove si origina, in particolare, nell'entroterra della Terra di Marie Byrd. Situato nella piatta pianura glaciale sita a nord del blocco dei monti Horlick, il flusso glaciale Horlick si muove verso ovest-sud-ovest parallelamente all'estensione dei suddetti monti e lungo il suo percorso viene arricchito dal flusso glaciale Shimizu e da altri suoi tributari, come il ghiacciaio Davisville, fino ad andare ad alimentare il ghiacciaio Reedy, nella parte orientale del territorio della Dipendenza di Ross. (it)
- 霍利克冰流(英語:Horlick Ice Stream),是南極洲的冰流,位於瑪麗伯德地,美國地質調查局根據測量和美國海軍拍攝的空中照片繪入地圖,現時由南極條約體系管理。 (zh)
- Der Horlick-Eisstrom ist ein großer Eisstrom im westantarktischen Marie-Byrd-Land. Im strukturlosen Norden des Hauptmassivs der Horlick Mountains fließt er parallel zu diesen in westsüdwestlicher Richtung zum unteren Abschnitt des Reedy-Gletschers. (de)
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| - Location of Horlick Ice Stream in Antarctica (en)
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| - Der Horlick-Eisstrom ist ein großer Eisstrom im westantarktischen Marie-Byrd-Land. Im strukturlosen Norden des Hauptmassivs der Horlick Mountains fließt er parallel zu diesen in westsüdwestlicher Richtung zum unteren Abschnitt des Reedy-Gletschers. Das Gebiet wurde vom United States Geological Survey und mithilfe von Luftaufnahmen der United States Navy von 1960 bis 1964 kartografisch erfasst. Das Advisory Committee on Antarctic Names benannte ihn 1967 in Verbindung mit den Horlick Mountains nach dem Unternehmer (1846–1936), einem Sponsoren der zweiten Antarktisexpedition (1933–1935) des US-amerikanischen Polarforschers Richard Evelyn Byrd. (de)
- Horlick Ice Stream (85°17′S 132°00′W / 85.283°S 132.000°W) is a large ice stream on the featureless ice surface to the north of the main mass of the Horlick Mountains of Antarctica, draining west-southwestward, parallel to these mountains, to enter the lower portion of the Reedy Glacier. It was mapped by the U.S. Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names in association with the Horlick Mountains. (en)
- Il flusso di ghiaccio Horlick è un flusso di ghiaccio lungo oltre 100 km situato in Antartide, dove si origina, in particolare, nell'entroterra della Terra di Marie Byrd. Situato nella piatta pianura glaciale sita a nord del blocco dei monti Horlick, il flusso glaciale Horlick si muove verso ovest-sud-ovest parallelamente all'estensione dei suddetti monti e lungo il suo percorso viene arricchito dal flusso glaciale Shimizu e da altri suoi tributari, come il ghiacciaio Davisville, fino ad andare ad alimentare il ghiacciaio Reedy, nella parte orientale del territorio della Dipendenza di Ross. (it)
- 霍利克冰流(英語:Horlick Ice Stream),是南極洲的冰流,位於瑪麗伯德地,美國地質調查局根據測量和美國海軍拍攝的空中照片繪入地圖,現時由南極條約體系管理。 (zh)
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