The deep crack in the Antarctica's Larsen C ice shelf continues to cut across the ice.
While the iceberg remains attached to the ice shelf, its outer end is moving at the highest speed ever recorded on this ice shelf.
It has tripled in speed to more than ten metres per day between June 24 and 27, according to scientists of Project MIDAS, a UK-based Antarctic research project.
Monitored by the Copernicus Sentinel-1 radar pair, the crack in the ice is now around 200 kilometres (km) long, leaving just five km between the end of the fissure and the ocean.
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European Space Agency's (ESA) CryoSat Earth Explorer satellite carries a radar altimeter that will measure the height of the ice surface before the 6,000 square kilometre iceberg is spawned.
The information is used to work out how the thickness of sea ice and land ice is changing and, consequently, how the volume of Earth's ice is being affected by the climate.
"We have also estimated that the depth below sea level could be as much as 210 metres," Gourmelen said.
Icebergs calve from Antarctica all the time, but because this one is particularly large, its path across the ocean needs to be monitored as it could pose a hazard to maritime traffic.
An iceberg, similar in size, drifted around the Brunt ice shelf in December 2015, causing alarm for those stationed at the Halley research base, which sits on the floating section of the shelf.
"As for this new Larsen C berg, we are not sure what will happen. It could, in fact, even calve in pieces or break up shortly after," Hogg said.
"Whole or in pieces, ocean currents could drag it north, even as far as the Falkland Islands. If so it could pose a hazard for ships in Drake Passage," she said.
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