Larsen Ice Shelf

Parts of the Larsen Ice Shelf broke up in recent decades.

Around the same time, the Larsen Ice Shelf divested itself of a huge projection.

Skvarca and his team were the last people to set foot on the northern part of the Larsen Ice Shelf.

Larsen Ice Shelf Antarctica's most conspicuous geographical feature is ice.

Larsen Ice Shelf.

Formed in 2002 as a result of the disintegration of Larsen Ice Shelf in the area.

Fahrbach et al. propose that low-salinity bottom water is formed near the Larsen Ice Shelf.

The Larsen Ice Shelf is "typical" in that it is primarily fed by a land-based glacier.

February 16: Scientists find over 20 new species of animals as the Larsen Ice Shelf breaks in the Antarctic.

Hulbe, C. Larsen Ice Shelf 2002: Warmest summer on record leads to disintegration.

In finer detail, the Larsen Ice Shelf is a series of three shelves that occupy (or occupied) distinct embayments along the coast.

The peninsula is surrounded by the Larsen Ice Shelf, which is part of the Weddell Sea.

In December 1893 he also became the first person to ski in Antarctica where the Larsen Ice Shelf was named after him.

The peninsula has a sharp elevation gradient, with glaciers flowing into the Larsen Ice Shelf, which experienced significant breakup in 2002.

Just north of Thuronyi Bluff, the Larsen Ice Shelf once extended a hundred kilometers (or more) from land before any open sea would be encountered.

"Break up of the Larsen Ice Shelf, Antarctica", NASA Earth Observatory.

The feature is a useful landmark along a proven east-west route from Larsen Ice Shelf across Bruce Plateau, Graham Land.

Two sections of Antarctica's Larsen Ice Shelf broke apart into hundreds of unusually small fragments (hundreds of meters wide or less) in 1995 and 2002.

Most of the sea, especially in the south, is covered by huge sheets of ice, the largest of which are the Ronne, Filchner, and Larsen ice shelves.

The most dramatic example of glacier retreat on the continent is the loss of large sections of the Larsen Ice Shelf on the Antarctic Peninsula.

It was formed as a result of the break-up of Larsen Ice Shelf in the area, and the retreat of Pequod Glacier in the early 21st century.

It leads from Mobiloil Inlet to Larsen Ice Shelf between Cape Keeler and Cape Mayo.

The Seal Nunataks are a group of 16 nunataks emerging from the Larsen Ice Shelf east of Graham Land, Antarctic Peninsula.

The northernmost section of the Larsen Ice Shelf Complex, called Larsen A, lost about 1,500 square kilometers of ice in an abrupt event in January 1995.

In contrast to the some other ice shelves on the Antarctic Peninsula, for example the Larsen Ice Shelf, the Stange Ice Shelf has been relatively stable.