Gerasimou Glacier

Gerasimou Glacier (84°42′S 177°3′W) is a steep-walled tributary glacier, 5 nautical miles (9 km) long, entering the west side of Shackleton Glacier opposite the Gemini Nunataks, in the Queen Maud Mountains of Antarctica. It was named by the Texas Tech Shackleton Glacier Expedition, 1964–65, for Helen Gerasimou, a polar personnel specialist with the Office of Antarctic Programs, National Science Foundation.[1]

References

"Gerasimou Glacier". Geographic Names Information System. United States Geological Survey. Retrieved 2012-04-22.

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