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The Larsen Ice Shelf is a long ice shelf in the northwest part of the Weddell Sea, extending along the east coast of the Antarctic Peninsula [1] from Cape Longing to Smith Peninsula. It is named after Captain Carl Anton Larsen , the master of the Norwegian whaling vessel Jason , who sailed along the ice front as far as 68°10' South during ...
The calving of A-68 reduced the overall size of the Larsen C shelf by 12 percent. [5] [6] Historical data shows that many icebergs that break off from the Antarctic Peninsula reach South Georgia and the South Sandwich Islands. [7] The name "A-68" was assigned by the US National Ice Center. It broke into parts with the mother berg dubbed A-68A.
This is a list of Antarctic ice shelves.. An image of Antarctica differentiating its landmass (dark grey) from its ice shelves (minimum extent, light grey, and maximum extent, white) Edge of Ekstrom Ice Shelf
When A-68 broke off of Larsen C earlier this year, it was a historic event. A-68 is one of the largest icebergs ever to break off Antarctica. NASA released amazing close-up images of the giant new ...
A fast moving crack in an ice shelf in Antarctica could create one of the largest icebergs ever recorded. Antarctic ice shelf crack grows 11 miles and will create one of the largest icebergs ever ...
An ice shelf the size of New York City has collapsed in East Antarctica, an area long thought to be stable and not hit much by climate change, concerned scientists said Friday. The collapse ...
The split of the A38-B iceberg is recorded in this series of images. The iceberg was originally part of the massive A-38 iceberg, which broke from the Ronne Ice Shelf in Antarctica [3] B-15A: 6,400 2002 Northern edge of Iceberg B-15A in the Ross Sea, Antarctica, 29 January 2002: A-68: 5,800 175 50 2017 Calving crack in the Larsen C ice shelf [2 ...
Some named Antarctic iceshelves. Ice shelf extending approximately 6 miles into the Antarctic Sound from Joinville Island. An ice shelf is "a floating slab of ice originating from land of considerable thickness extending from the coast (usually of great horizontal extent with a very gently sloping surface), resulting from the flow of ice sheets, initially formed by the accumulation of snow ...