Brunner Glacier

Brunner Glacier (85°14′S 175°38′W) is a narrow steep-walled glacier 2 nautical miles (4 km) long, descending the west slope of the Cumulus Hills between Landry Bluff and Halfmoon Bluff to enter Shackleton Glacier. It was named by the Texas Tech Shackleton Glacier Expedition (1964–65) for Staff Sergeant Donald R. Brunner, a member of the U.S. Army Aviation Detachment which supported the expedition.[1]

References

"Brunner Glacier". Geographic Names Information System. United States Geological Survey. Retrieved 2011-09-22.

This article incorporates public domain material from the United States Geological Survey document: "Brunner 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 P-form Ribbon lake Roche moutonnée Suncup 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
Glaciofluvial	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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