Burgess Glacier
Mill Glacier is a tributary glacier, 10 nautical miles wide, flowing northwest between the Dominion Range and the Supporters Range into Beardmore Glacier, Antarctica.Places of Interest
Highlights include Otway Massif and Mount Petlock.
Otway Massif
Peak
The Grosvenor Mountains are a group of widely scattered mountains and nunataks rising above the Antarctic polar plateau east of the head of Mill Glacier, extending from Mount Pratt in the north to the Mount Raymond area in the south, and from Otway Massif in the northwest to Larkman Nunatak in the southeast.
Mount Petlock
Peak
The Grosvenor Mountains are a group of widely scattered mountains and nunataks rising above the Antarctic polar plateau east of the head of Mill Glacier, extending from Mount Pratt in the north to the Mount Raymond area in the south, and from Otway Massif in the northwest to Larkman Nunatak in the southeast. Mount Petlock is situated 3½ km northeast of Burgess Glacier.
Mount Spohn
Peak
The Grosvenor Mountains are a group of widely scattered mountains and nunataks rising above the Antarctic polar plateau east of the head of Mill Glacier, extending from Mount Pratt in the north to the Mount Raymond area in the south, and from Otway Massif in the northwest to Larkman Nunatak in the southeast. Mount Spohn is situated 4 km south of Burgess Glacier.
Burgess Glacier
- Type: Glacier with an elevation of 2,378 metres
- Category: landform
- Location: Antarctica
- View on OpenStreetMap
Latitude
-85.43333° or 85° 26′ southLongitude
171.91667° or 171° 55′ eastElevation
2,378 metres (7,802 feet)Open location code
2V6HHW88+MMGeoNames ID
6630564
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Satellite Map
Discover Burgess Glacier from above in high-definition satellite imagery.
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Highlights include Johnston Heights and Mom Peak.
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