Law Glacier

Law Glacier (84°5′S 161°0′E / 84.083°S 161.000°E / -84.083; 161.000Coordinates: 84°5′S 161°0′E / 84.083°S 161.000°E / -84.083; 161.000) is a glacier about 10 nautical miles (20 km) wide between the south end of the Queen Elizabeth Range and the MacAlpine Hills, gradually descending east-northeast from the Antarctic polar plateau to Bowden Névé. It was named by the New Zealand party of the Commonwealth Trans-Antarctic Expedition (1956–58) for B.R. Law, Deputy-Chairman of the Ross Sea Committee.^[1]

References

↑ "Law Glacier". Geographic Names Information System. United States Geological Survey. Retrieved 2013-06-05.

This article incorporates public domain material from the United States Geological Survey document "Law 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

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