This bay no longer exists, engulfed by the ice of the Amery Ice Shelf.

These fractures threaten to break off a 1000 square kilometre piece of the Amery Ice Shelf.

Exploration and mapping of the southwestern (interior) side of the Amery Ice Shelf was accomplished by Australian expeditions during the 1950s.

They were discovered by the Australian National Antarctic Research Expeditions southern party of 1956-57 and so named because of their proximity to the Amery Ice Shelf.

Sandefjord Bay was an ice bay at the head of Prydz Bay, lying on the eastern side of the Amery Ice Shelf.

Lambert Glacier flows from Lambert Graben into the Amery Ice Shelf on the southwest side of Prydz Bay.

MacKenzie Bay is a relatively small embayment of the western extremity of the Amery Ice Shelf, about 20 miles northeast of Foley Promontory.

It drains 8% of the Antarctic ice sheet to the east and south of the Prince Charles Mountains and flows northward to the Amery Ice Shelf.

Jetty Peninsula is an elongated, steep-sided, almost flat-topped peninsula that extends northward from just east of Beaver Lake for about 30 miles into the Amery Ice Shelf.

The Amery Ice Shelf is small compared to the Ross Ice Shelf and the Filchner-Ronne Ice Shelf.

Thil Island is a small rocky island lying 1 nautical mile (1.9 km) northeast of Jennings Promontory in the eastern part of the Amery Ice Shelf.

The world's longest glacier drains about 8% of the Antarctic ice sheet and is up to 400km long and 200km wide at the point where it reaches the Amery Ice Shelf.

Sighted on a flight by an ANARE (Australian National Antarctic Research Expeditions) Beaver aircraft over the Amery Ice Shelf on November 2, 1957.

The sound of the second wave dwindled into the distance, and when asked by an aide, he approved of the departure of the third wave toward the Amery Ice Shelf and the Ingrid Christensen coast.

Dr. Warren compared the oxygen isotope ratios of small samples taken from the upper and lower portions of a green iceberg that had broken off the Amery Ice Shelf and floated toward the south Indian Ocean.

The group was named by the Antarctic Names Committee of Australia for M.J. Corry, leader and glaciologist of the Amery Ice Shelf party in 1968, who took part in the survey.

The ice here is flowing at about 500 m per year, but velocities of over 1200 m per year are known at the edge of the Amery Ice Shelf, which is fed by this gigantic stream of ice.

In December 2006, it was reported by the Australian Broadcasting Corporation that Australian scientists were heading to the Amery Ice Shelf to investigate enormous cracks that had been forming for over a decade at a rate of three to five metres a day.

It is bounded on the west by Amery Ice Shelf, Mac.

It is aligned north-south and lies in the eastern part of Amery Ice Shelf.

These fractures threaten to break off a 1000 square kilometre piece of the Amery Ice Shelf.

This bay no longer exists, engulfed by the ice of the Amery Ice Shelf.

Breakout of a large part of Amery Ice Shelf has drastically reduced the size of this feature; in 1968 the bay was 15 miles wide.

Exploration and mapping of the southwestern (interior) side of the Amery Ice Shelf was accomplished by Australian expeditions during the 1950s.

Rubeli Bluff is a bluff on the north end of the Reinbolt Hills, at the east margin of Amery Ice Shelf.

MacKenzie Bay is a relatively small embayment of the western extremity of the Amery Ice Shelf, about 20 miles northeast of Foley Promontory.

They were discovered by the Australian National Antarctic Research Expeditions southern party of 1956-57 and so named because of their proximity to the Amery Ice Shelf.

Lambert Glacier flows from Lambert Graben into the Amery Ice Shelf on the southwest side of Prydz Bay.

Sandefjord Bay was an ice bay at the head of Prydz Bay, lying on the eastern side of the Amery Ice Shelf.

The Amery Ice Shelf is small compared to the Ross Ice Shelf and the Filchner-Ronne Ice Shelf.

It is located on the south-west part of Sandefjord Bay adjacent to Amery Ice Shelf, about 26 km west of Mount Caroline Mikkelsen.

So named because of its proximity to the landing place for stores and equipment for the ANARE Amery Ice Shelf party in January-March, 1968.

Jetty Peninsula is an elongated, steep-sided, almost flat-topped peninsula that extends northward from just east of Beaver Lake for about 30 miles into the Amery Ice Shelf.

It drains 8% of the Antarctic ice sheet to the east and south of the Prince Charles Mountains and flows northward to the Amery Ice Shelf.

Thil Island is a small rocky island lying 1 nautical mile (1.9 km) northeast of Jennings Promontory in the eastern part of the Amery Ice Shelf.

The world's longest glacier drains about 8% of the Antarctic ice sheet and is up to 400km long and 200km wide at the point where it reaches the Amery Ice Shelf.

Sighted on a flight by an ANARE (Australian National Antarctic Research Expeditions) Beaver aircraft over the Amery Ice Shelf on November 2, 1957.

Tester Nunatak is the southernmost of a group of three nunataks in the northern part of the Manning Nunataks, in the east part of Amery Ice Shelf.

The group was named by the Antarctic Names Committee of Australia for M.J. Corry, leader and glaciologist of the Amery Ice Shelf party in 1968, who took part in the survey.

The sound of the second wave dwindled into the distance, and when asked by an aide, he approved of the departure of the third wave toward the Amery Ice Shelf and the Ingrid Christensen coast.

Dr. Warren compared the oxygen isotope ratios of small samples taken from the upper and lower portions of a green iceberg that had broken off the Amery Ice Shelf and floated toward the south Indian Ocean.

In December 2006, it was reported by the Australian Broadcasting Corporation that Australian scientists were heading to the Amery Ice Shelf to investigate enormous cracks that had been forming for over a decade at a rate of three to five metres a day.

Named by Antarctic Names Committee of Australia (ANCA) for N. Linton-Smith, senior technical officer with the Antarctic Division, Melbourne, a member of the ANARE Amery Ice Shelf glaciological traverse in 1970.