Mill Stream Glacier

Mill Stream Glacier (85°20′S 171°0′E / 85.333°S 171.000°E / -85.333; 171.000Coordinates: 85°20′S 171°0′E / 85.333°S 171.000°E / -85.333; 171.000) is a tributary glacier, about 10 nautical miles (19 km) wide, flowing west between the Supporters Range and Otway Massif in Antarctica to enter Mill Glacier. It was named by the New Zealand Geological Survey Antarctic Expedition of 1961–62 in association with Mill Glacier.^[1]

References

↑ "Mill Stream Glacier". Geographic Names Information System. United States Geological Survey. Retrieved 2013-09-25.

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