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Tomilin Glacier
Glacier in Antarctica
Glacier in Antarctica
| Field | Value |
|---|---|
| type | Outlet glacier |
| location | East Antarctica |
| map | Antarctica |
| map_caption | Location within Antarctica |
| coordinates | |
| length | 15 nmi |
| thickness | unknown |
| terminus | Southern Ocean |
| status | unknown |
The Tomilin Glacier () is a glacier over 15 nmi long, draining north from Pope Mountain in the central Wilson Hills. It enters the sea east of Goodman Hills and Cape Kinsey, forming a substantial glacier tongue.
Discovery and naming
The Tomilin Glacier was photographed from aircraft of the United States Navy Operation Highjump in 1947, and by the Soviet Antarctic Expedition 1958. It was named by the latter for Soviet polar aviator Mikhail N. Tomilin (1908-52), who perished in the Arctic.
Location
The Tomilin Glacier forms in the Wilson Hills, flowing north or northeast from Governor Mountain and Pope Mountain, and passing Feeney Ridge, Serba Peak, Axthelm Ridge and Parkinson Peak to the east. It is joined from the west by Walsh Glacier, just north of Schmehl Peak, and flows north past the Goodman Hills to enter the ocean in an ice tongue. It is joined from the southeast by Noll Glacier, which forms near Wegert Bluff and flows northwest past Clarke Bluff, where it is joined by Fergusson Glacier, past Burt Rocks and Axtberm Ridge before joining Tomilin Glacier at Parkinson Point.
Tributaries
Walsh Glacier
Noll Glacier
Fergusson Glacier
Features

Feeney Ridge
Serba Peak
Axthelm Ridge
Parkinson Peak
Schmehl Peak
Wegert Bluff
Clarke Bluff
Burt Rocks
References
Sources
- {{citation|url=https://pubs.usgs.gov/fedgov/70039167/report.pdf |accessdate=2023-12-03 |edition=2 |editor-last=Alberts |title=Geographic Names of the Antarctic |editor-first=Fred G.
- {{citation |url=https://commons.wikimedia.org/wiki/File:C69198s1_Suvorov_Glacier.jpg |accessdate=2024-01-19
This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.
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