Canham Glacier (71°49′S 163°0′E / 71.817°S 163.000°E) is a tributary glacier about 30 nautical miles (60 km) long which drains the northwest part of Evans Neve in Antarctica. The glacier drains northwest between the Alamein Range and the Salamander Range of the Freyberg Mountains and enters the Rennick Glacier westward of Bowers Peak, Victoria Land. The geographical feature was first mapped by the United States Geological Survey from surveys and from U.S. Navy air photos, 1960–62, and named by the Advisory Committee on Antarctic Names for Lieutenant Commander , officer in charge of the winter party at the , McMurdo Sound, 1956. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
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| - Canham-Gletscher (de)
- Canham Glacier (en)
- Ghiacciaio Canham (it)
- Canham Glacier (sv)
- 坎漢冰川 (zh)
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| - Canham Glacier (71°49′S 163°0′E / 71.817°S 163.000°E) is a tributary glacier about 30 nautical miles (60 km) long which drains the northwest part of Evans Neve in Antarctica. The glacier drains northwest between the Alamein Range and the Salamander Range of the Freyberg Mountains and enters the Rennick Glacier westward of Bowers Peak, Victoria Land. The geographical feature was first mapped by the United States Geological Survey from surveys and from U.S. Navy air photos, 1960–62, and named by the Advisory Committee on Antarctic Names for Lieutenant Commander , officer in charge of the winter party at the , McMurdo Sound, 1956. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare. (en)
- Il ghiacciaio Canham è un ghiacciaio lungo circa 60 km situato sulla costa di Oates, nella regione nord-occidentale della Dipendenza di Ross, in Antartide. In particolare, il ghiacciaio, il cui punto più alto si trova a circa 2000 m s.l.m., ha origine dal versante nord-occidentale del nevaio Evans e da qui fluisce verso nord-ovest scorrendo tra la dorsale Alamein e la dorsale Salamander, nelle montagne di Freyberg, fino ad unire il proprio flusso, a cui lungo il percorso di uniscono quelli di diversi tributari, tra cui il ghiacciaio Hoshko, a quello del ghiacciaio Rennick, a nord dell'estremità settentrionale della sopraccitata dorsale Alamein. (it)
- Canham Glacier är en glaciär i Antarktis. Den ligger i Östantarktis. Nya Zeeland gör anspråk på området. Canham Glacier ligger 861 meter över havet. Terrängen runt Canham Glacier är varierad. Den högsta punkten i närheten är 1 808 meter över havet, 7,5 kilometer norr om Canham Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten. (sv)
- 坎漢冰川(英語:Canham Glacier)是南極洲的冰川,位於維多利亞地,全長約60公里,流經阿拉曼山脈和薩拉曼德山脈之間,最終在鮑爾斯峰以西注入雷尼克冰川。 (zh)
- Der Canham-Gletscher ist ein etwa 50 km langer Gletscher im ostantarktischen Viktorialand. Er fließt vom nordwestlichen Teil des Evans-Firnfelds zwischen der Alamein Range und der Salamander Range der Freyberg Mountains zum Rennick-Gletscher, den er westlich des Bowers Peak erreicht. (de)
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| - Canham Glacier (71°49′S 163°0′E / 71.817°S 163.000°E) is a tributary glacier about 30 nautical miles (60 km) long which drains the northwest part of Evans Neve in Antarctica. The glacier drains northwest between the Alamein Range and the Salamander Range of the Freyberg Mountains and enters the Rennick Glacier westward of Bowers Peak, Victoria Land. The geographical feature was first mapped by the United States Geological Survey from surveys and from U.S. Navy air photos, 1960–62, and named by the Advisory Committee on Antarctic Names for Lieutenant Commander , officer in charge of the winter party at the , McMurdo Sound, 1956. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare. (en)
- Der Canham-Gletscher ist ein etwa 50 km langer Gletscher im ostantarktischen Viktorialand. Er fließt vom nordwestlichen Teil des Evans-Firnfelds zwischen der Alamein Range und der Salamander Range der Freyberg Mountains zum Rennick-Gletscher, den er westlich des Bowers Peak erreicht. Das Gebiet wurde durch Vermessungsarbeiten des United States Geological Survey und mithilfe von Luftaufnahmen der United States Navy von 1960 bis 1962 kartografisch erfasst. Das Advisory Committee on Antarctic Names benannte den Gletscher 1964 nach Lieutenant Commander David W. Canham Jr. (1920–1986), diensthabender Offizier der Flugbereitschaft der United States Navy am McMurdo-Sund im Jahr 1956. (de)
- Il ghiacciaio Canham è un ghiacciaio lungo circa 60 km situato sulla costa di Oates, nella regione nord-occidentale della Dipendenza di Ross, in Antartide. In particolare, il ghiacciaio, il cui punto più alto si trova a circa 2000 m s.l.m., ha origine dal versante nord-occidentale del nevaio Evans e da qui fluisce verso nord-ovest scorrendo tra la dorsale Alamein e la dorsale Salamander, nelle montagne di Freyberg, fino ad unire il proprio flusso, a cui lungo il percorso di uniscono quelli di diversi tributari, tra cui il ghiacciaio Hoshko, a quello del ghiacciaio Rennick, a nord dell'estremità settentrionale della sopraccitata dorsale Alamein. (it)
- Canham Glacier är en glaciär i Antarktis. Den ligger i Östantarktis. Nya Zeeland gör anspråk på området. Canham Glacier ligger 861 meter över havet. Terrängen runt Canham Glacier är varierad. Den högsta punkten i närheten är 1 808 meter över havet, 7,5 kilometer norr om Canham Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten. (sv)
- 坎漢冰川(英語:Canham Glacier)是南極洲的冰川,位於維多利亞地,全長約60公里,流經阿拉曼山脈和薩拉曼德山脈之間,最終在鮑爾斯峰以西注入雷尼克冰川。 (zh)
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