Montgomerie Glacier

Montgomerie Glacier (83°47′S 166°55′E / 83.783°S 166.917°E / -83.783; 166.917Coordinates: 83°47′S 166°55′E / 83.783°S 166.917°E / -83.783; 166.917) is a narrow tributary glacier, 10 nautical miles (19 km) long, flowing north along the west side of Hampton Ridge in the Queen Alexandra Range of Antarctica to enter Lennox-King Glacier. It was named by the Northern Party of the New Zealand Geological Survey Antarctic Expedition of 1961–62 for John Montgomerie, assistant surveyor of that party.^[1]

References

↑ "Montgomerie Glacier". Geographic Names Information System. United States Geological Survey. Retrieved 2013-11-01.

This article incorporates public domain material from the United States Geological Survey document "Montgomerie Glacier" (content from the Geographic Names Information System).

Types

Anatomy

Processes

Measurements

Volcanic relations

Erosional	Arête Cirque Cirque stairway Crag and tail Finger lake Fjord Glacial horn Glacial lake Glacial striae Hanging valley Ribbon lake Roche moutonnée Tarn Trough lake Trough valley Tunnel valley U-valley Valley step Zungenbecken
Depositional	Drumlin Erratic block Moraine Moraine-dammed lake Pulju moraine Rogen moraine Sevetti moraine Terminal moraine Till plain Veiki moraine
Glacifluvial	Alpentor Diluvium Esker Giant current ripples Kame Kame delta Kettle hole Outwash fan Sandur Urstromtal

Glaciology
Category
List
Template:Periglacial environment

Glaciers in the Antarctic

Glaciers of the Ross Dependency

King Edward VII Land

Ross Dependency

This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.