Keltie Glacier

Keltie Glacier is a large Antarctic glacier, 30 nautical miles (56 km) long, draining from Pain Névé southwest around the southern extremity of the Commonwealth Range, and then northwest to enter Beardmore Glacier at Ranfurly Point. It was discovered by the British Antarctic Expedition, 1907–09, under Ernest Shackleton, who named it for Sir John Scott Keltie, Secretary of the Royal Geographical Society, 1892–1915.[1]

NASA Radarsat Image of Antarctic Glaciers Showing Keltie Glacier

See also

List of glaciers in the Antarctic

References

"Keltie Glacier". Geographic Names Information System. United States Geological Survey. Retrieved 2013-04-22.

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