Ashworth Glacier

Ashworth Glacier
Location of Ashworth Glacier in Antarctica
Location	Ross Dependency
Coordinates	85°01′36″S 169°15′53″E / 85.02667°S 169.26472°E / -85.02667; 169.26472
Terminus	Mill Glacier

Ashworth Glacier (85°01′36″S 169°15′53″E / 85.02667°S 169.26472°E / -85.02667; 169.26472Coordinates: 85°01′36″S 169°15′53″E / 85.02667°S 169.26472°E / -85.02667; 169.26472) is an Antarctic glacier with sharply delineated sides, flowing west from Supporters Range into Mill Glacier, 5 kilometres (3 mi) north of Mount Iveagh. It was named by the Advisory Committee on Antarctic Names in 2007, after Allan C. Ashworth, Professor of Paleontology and Stratigraphy at North Dakota State University. He discovered the only yet known fly and beetle fossils in Antarctica in the nearby Dominion Range.

See also

References

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