Koski Glacier

Koski Glacier (85°17′S 167°15′E / 85.283°S 167.250°E / -85.283; 167.250Coordinates: 85°17′S 167°15′E / 85.283°S 167.250°E / -85.283; 167.250) is an east-flowing glacier, 7 nautical miles (13 km) long, draining the east-central portion of the Dominion Range icecap, Antarctica. The glacier lies close north of Vandament Glacier, whose flow it parallels, and terminates at Mill Glacier just southeast of Browns Butte. It was named by the Advisory Committee on Antarctic Names for Raymond J. Koski, a United States Antarctic Research Program engineer on several traverses originating at the South Pole Station 1962–63, 1963–64 and 1964–65.^[1]

References

↑ "Koski Glacier". Geographic Names Information System. United States Geological Survey. Retrieved 2013-05-16.

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