The McIntosh Cliffs are a line of steep, uneven, volcanic bluffs or cliffs, 16 nautical miles (30 km) long, forming the southwest side of the Minna Bluff peninsula, at the northeast end of Hillary Coast, Ross Dependency, Antarctica. The height of the cliffs increases from west to east, ranging from 400 to 600 metres (1,300 to 2,000 ft) above the Ross Ice Shelf. They were named by the Advisory Committee on Antarctic Names in 1999 after of the Department of Geoscience, New Mexico Institute of Mining and Technology (NMIMT), Socorro, a member of the 1982 NMIMT field party that carried out the first geological mapping of Minna Bluff. McIntosh did additional field work at Mount Erebus, 1977–78, 1984–85; Mount Discovery and Mason Spur, 1983–84; Mount Murphy, 1985; the Executive Committee Range,
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| - McIntosh-Kliffs (de)
- McIntosh Cliffs (en)
- 麥金托什崖 (zh)
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| - Die McIntosh-Kliffs sind eine Reihe steiler und ungleichmäßiger Kliffs vulkanischen Ursprungs an der Scott-Küste des ostantarktischen Viktorialands. Sie erstrecken sich über eine Länge von 26 km an der Südwestseite des Minna Bluff. Ihre Höhe variiert zwischen 400 m im Westen und 600 m an ihrem östlichen Ende. Das Advisory Committee on Antarctic Names benannte sie 1999 nach dem US-amerikanischen Geologen William C. McIntosh vom in Socorro, der 1982 an der erstmaligen geologischen Kartierung des Minna Bluff beteiligt und auch in weiteren Kampagnen in Antarktika tätig war. (de)
- 麥金托什崖（英語：McIntosh Cliffs），是南極洲的山崖，位於維多利亞地的希拉里海岸東北端，處於明納海崖西南面，長30公里，現時由南極條約體系管理。 (zh)
- The McIntosh Cliffs are a line of steep, uneven, volcanic bluffs or cliffs, 16 nautical miles (30 km) long, forming the southwest side of the Minna Bluff peninsula, at the northeast end of Hillary Coast, Ross Dependency, Antarctica. The height of the cliffs increases from west to east, ranging from 400 to 600 metres (1,300 to 2,000 ft) above the Ross Ice Shelf. They were named by the Advisory Committee on Antarctic Names in 1999 after of the Department of Geoscience, New Mexico Institute of Mining and Technology (NMIMT), Socorro, a member of the 1982 NMIMT field party that carried out the first geological mapping of Minna Bluff. McIntosh did additional field work at Mount Erebus, 1977–78, 1984–85; Mount Discovery and Mason Spur, 1983–84; Mount Murphy, 1985; the Executive Committee Range, (en)
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| - Die McIntosh-Kliffs sind eine Reihe steiler und ungleichmäßiger Kliffs vulkanischen Ursprungs an der Scott-Küste des ostantarktischen Viktorialands. Sie erstrecken sich über eine Länge von 26 km an der Südwestseite des Minna Bluff. Ihre Höhe variiert zwischen 400 m im Westen und 600 m an ihrem östlichen Ende. Das Advisory Committee on Antarctic Names benannte sie 1999 nach dem US-amerikanischen Geologen William C. McIntosh vom in Socorro, der 1982 an der erstmaligen geologischen Kartierung des Minna Bluff beteiligt und auch in weiteren Kampagnen in Antarktika tätig war. (de)
- The McIntosh Cliffs are a line of steep, uneven, volcanic bluffs or cliffs, 16 nautical miles (30 km) long, forming the southwest side of the Minna Bluff peninsula, at the northeast end of Hillary Coast, Ross Dependency, Antarctica. The height of the cliffs increases from west to east, ranging from 400 to 600 metres (1,300 to 2,000 ft) above the Ross Ice Shelf. They were named by the Advisory Committee on Antarctic Names in 1999 after of the Department of Geoscience, New Mexico Institute of Mining and Technology (NMIMT), Socorro, a member of the 1982 NMIMT field party that carried out the first geological mapping of Minna Bluff. McIntosh did additional field work at Mount Erebus, 1977–78, 1984–85; Mount Discovery and Mason Spur, 1983–84; Mount Murphy, 1985; the Executive Committee Range, 1989–90; and the Crary Mountains, 1992–93. (en)
- 麥金托什崖（英語：McIntosh Cliffs），是南極洲的山崖，位於維多利亞地的希拉里海岸東北端，處於明納海崖西南面，長30公里，現時由南極條約體系管理。 (zh)
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