Michigan Plateau (86°8′S 133°30′W / 86.133°S 133.500°W) is an undulating ice-covered plateau, 30 nautical miles (56 km) long, which rises to 3,000 metres (10,000 ft) at the western side of Reedy Glacier, Antarctica. The northern and eastern sides of the plateau are marked by the steep Watson Escarpment; the western and southern sides grade gradually to the elevation of the interior ice. It was mapped by the United States Geological Survey from ground surveys and U.S. Navy aerial photography, 1960–64, and was named by the Advisory Committee on Antarctic Names after the University of Michigan at Ann Arbor, which has sent numerous research personnel to work in Antarctica.
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| - Michigan-Plateau (de)
- Michigan Plateau (it)
- Michigan Plateau (en)
- Michigan Plateau (sv)
- 密歇根高原 (zh)
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| - Michigan Plateau (86°8′S 133°30′W / 86.133°S 133.500°W) is an undulating ice-covered plateau, 30 nautical miles (56 km) long, which rises to 3,000 metres (10,000 ft) at the western side of Reedy Glacier, Antarctica. The northern and eastern sides of the plateau are marked by the steep Watson Escarpment; the western and southern sides grade gradually to the elevation of the interior ice. It was mapped by the United States Geological Survey from ground surveys and U.S. Navy aerial photography, 1960–64, and was named by the Advisory Committee on Antarctic Names after the University of Michigan at Ann Arbor, which has sent numerous research personnel to work in Antarctica. (en)
- Michigan Plateau är en platå i Antarktis. Den ligger i den centrala delen av kontinenten. Inget land gör anspråk på området. (sv)
- 密歇根高原（英語：Michigan Plateau）是南極洲的高原，位於瑪麗伯德地，長56公里，處於里迪冰川西面，海拔高度3,000米，根據美國地質調查局的測量和美國海軍的空中照片被繪入地圖。 (zh)
- Das Michigan-Plateau ist ein eisbedecktes, wellenförmiges Hochplateau von rund 50 km Länge im westantarktischen Marie-Byrd-Land. Es erhebt sich bis zu 3000 m hoch an der Westflanke des Reedy-Gletschers. Die Nord- und Ostseite sind durch das steilwandige Watson Escarpment markiert. Die West- und Südflanke steigen bis auf das Niveau des zentralen Polarplateaus an. (de)
- Il Michigan Plateau è un altopiano antartico, ondulato e coperto di ghiaccio, lungo 56 km, situato a circa 3.000 m di altitudine sul fianco occidentale del Ghiacciaio Reedy, nei Monti della Regina Maud, in Antartide. I fianchi settentrionale e orientale del Michigan Plateau sono caratterizzati dalle ripide pareti rocciose del Watson Escarpment; invece i fianchi occidentale e meridionale degradano dolcemente fino all'altezza del ghiaccio dell'Altopiano Antartico. (it)
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| - Das Michigan-Plateau ist ein eisbedecktes, wellenförmiges Hochplateau von rund 50 km Länge im westantarktischen Marie-Byrd-Land. Es erhebt sich bis zu 3000 m hoch an der Westflanke des Reedy-Gletschers. Die Nord- und Ostseite sind durch das steilwandige Watson Escarpment markiert. Die West- und Südflanke steigen bis auf das Niveau des zentralen Polarplateaus an. Kartografisch erfasst wurde das Gebiet durch den United States Geological Survey und durch Luftaufnahmen der United States Navy aus den Jahren 1960 bis 1964. Das Advisory Committee on Antarctic Names benannte es 1967 nach der University of Michigan, die zahlreiche Wissenschaftler für Forschungsarbeiten in Antarktika entsendet hatte. (de)
- Michigan Plateau (86°8′S 133°30′W / 86.133°S 133.500°W) is an undulating ice-covered plateau, 30 nautical miles (56 km) long, which rises to 3,000 metres (10,000 ft) at the western side of Reedy Glacier, Antarctica. The northern and eastern sides of the plateau are marked by the steep Watson Escarpment; the western and southern sides grade gradually to the elevation of the interior ice. It was mapped by the United States Geological Survey from ground surveys and U.S. Navy aerial photography, 1960–64, and was named by the Advisory Committee on Antarctic Names after the University of Michigan at Ann Arbor, which has sent numerous research personnel to work in Antarctica. (en)
- Il Michigan Plateau è un altopiano antartico, ondulato e coperto di ghiaccio, lungo 56 km, situato a circa 3.000 m di altitudine sul fianco occidentale del Ghiacciaio Reedy, nei Monti della Regina Maud, in Antartide. I fianchi settentrionale e orientale del Michigan Plateau sono caratterizzati dalle ripide pareti rocciose del Watson Escarpment; invece i fianchi occidentale e meridionale degradano dolcemente fino all'altezza del ghiaccio dell'Altopiano Antartico. Il plateau è stato mappato dall'United States Geological Survey (USGS) sulla base di rilevazioni e foto aeree scattate dalla U.S. Navy nel periodo 1960-64. La denominazione è stata assegnata dall'Advisory Committee on Antarctic Names (US-ACAN) in onore dei molti dipartimenti dell'Università del Michigan che hanno inviato numerosi studiosi a compiere ricerche in Antartide. (it)
- Michigan Plateau är en platå i Antarktis. Den ligger i den centrala delen av kontinenten. Inget land gör anspråk på området. (sv)
- 密歇根高原（英語：Michigan Plateau）是南極洲的高原，位於瑪麗伯德地，長56公里，處於里迪冰川西面，海拔高度3,000米，根據美國地質調查局的測量和美國海軍的空中照片被繪入地圖。 (zh)
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