Tate Glacier

Tate Glacier (85°54′S 160°50′W) is a tributary glacier on the south side of Thomas Spur, flowing east and merging with Moffett Glacier just east of the spur where the two glaciers enter the larger Amundsen Glacier, in the Queen Maud Mountains. Mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1960–64. Named by Advisory Committee on Antarctic Names (US-ACAN) for Robert Tate, geomagnetist-seismologist with the South Pole Station winter party, 1964.

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