Canyon Glacier

Canyon Glacier (83°57′S 175°25′E / 83.950°S 175.417°E / -83.950; 175.417Coordinates: 83°57′S 175°25′E / 83.950°S 175.417°E / -83.950; 175.417) is a narrow glacier, 35 nautical miles (65 km) long, flowing to the Ross Ice Shelf. It drains the northwest slopes of Mount Wexler and moves northward between steep canyon walls of the Separation Range and Hughes Range to join the ice shelf immediately west of Giovinco Ice Piedmont. The glacier was observed from nearby Mount Patrick by the New Zealand Alpine Club Antarctic Expedition (1959–60) who gave the descriptive name.^[1]

References

↑ "Canyon Glacier". Geographic Names Information System. United States Geological Survey. Retrieved 2011-10-24.

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