Filchner-Ronne Ice Shelf

The Filchner-Ronne Ice Shelf lies to the east of the peninsula.

Berkner is surrounded by the Filchner-Ronne Ice Shelf.

The Filchner ice shelf is the eastern part of the Filchner-Ronne ice shelf.

The Ronne-Filchner ice shelf is also known as the Filchner-Ronne ice shelf.

Various ice shelves, including the Filchner-Ronne Ice Shelf, fringe the Weddell sea.

Much of the southern part of the sea is permanent ice, the Filchner-Ronne Ice Shelf, which can be up to 600 m thick.

The region would not be visited again until 1911, when Wilhelm Filchner discovered the Filchner-Ronne Ice Shelf.

The northern boundary is formed by the Filchner-Ronne Ice Shelf on the west and by Coats Land on the east.

The world's largest ice shelves are the Ross Ice Shelf and the Filchner-Ronne Ice Shelf in Antarctica.

Named after the American explorer Lincoln Ellsworth, the base was located on the western coast of the Weddell Sea over Filchner-Ronne Ice Shelf.

The international Filchner-Ronne Ice Shelf Programme (FRISP) was initiated in 1973 to study the ice shelf.

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

Antarctic icebergs formed by breaking off from an ice shelf, such as the Ross Ice Shelf or Filchner-Ronne Ice Shelf, are typically tabular.

Its geographical features include Filchner-Ronne Ice Shelf and Berkner Island, the second largest island of Antarctica, as well as several other islands rising from the ice shelf.

Situated south of Weddell Sea and between longitudes 20 W and 80 W, stretching from Filchner-Ronne Ice Shelf to the South Pole.

Support Force Glacier is a major glacier in the Pensacola Mountains, draining northward between the Forrestal Range and Argentina Range to the Filchner-Ronne Ice Shelf.

The expedition entered the Weddell Sea and discovered Luitpold Coast and the Filchner-Ronne Ice Shelf, which Filchner had originally named after the German emperor Wilhelm II.

The West Antarctic Ice Sheet is drained into the sea by several large ice streams, most of which flow into either the Ross Ice Shelf, or the Filchner-Ronne Ice Shelf.

Even the Nature Geoscience article states: "Although early attention focused on the ice stream drainages feeding the large Ross and Filchner-Ronne ice shelves (Box 1), at present these areas are thickening at moderate rates (several centimetres per year) or are near balance."