Cooper Glacier

The Cooper Glacier (85°30′S 164°30′W) is a tributary glacier, 15 nautical miles (30 km) long, flowing northeast between Butchers Spur and the Quarles Range to enter the south side of Axel Heiberg Glacier, in the Queen Maud Mountains. It was discovered by R. Admiral Byrd on several plane flights to the Queen Maud Mountains in November 1929, and named by him for Kent Cooper, an official of the Associated Press.[1]

References

"Cooper Glacier". Geographic Names Information System. United States Geological Survey. Retrieved 2011-11-22.

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

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