Beardmore Glacier
Sign in to saveglacier in Antarctica
Key facts
- Type
- Valley glacier
- Location
- Queen Maud Mountains
- Length
- 200 km (125 mi)
- Width
- 40 km (25 mi)
- Thickness
- unknown
- Terminus
- Ross Ice Shelf
- Status
- unknown
via Wikipedia infobox
Wikidata facts
- Instance of
- valley glacier
- Continent
- Antarctica
- Image
- Dugdale and Murray Glacier - Antarctica.jpg
- Length
- 168
Show 5 more facts
- Commons category
- Beardmore Glacier
- terminus
- Ross Ice Shelf
- mountain range
- Transantarctic Mountains
- native label
- Beardmore Glacier
- P12749
- Erich Wasmann
via Wikidata · CC0
~14 min read
Encyclopedic overview
The Beardmore Glacier in Antarctica is one of the largest valley glaciers in the world, being 200 km (125 mi) long and having a width of 40 km (25 mi). It descends about 2,200 m (7,200 ft) from the Antarctic Plateau to the Ross Ice Shelf and is bordered by the Commonwealth Range of the Queen Maud Mountains on the eastern side and the Queen Alexandra Range of the Central Transantarctic Mountains on the western. Its mouth is east of the Lennox-King Glacier. It is northwest of the Ramsey Glacier.
Early exploration
Excerpted from Wikipedia’s “Beardmore Glacier” article, available under the CC BY-SA 4.0 licence.
On the map
22 mapped locations