An iceberg twice the size of the ACT could be just hours away from breaking off the Antarctic

The massive crack has been growing and lately the ice has started to move faster than it ever has. John Sonntag/IceBridge/NASA Goddard Space Flight Center

The 300-metre-thick iceberg that’s getting ready to break off Antarctica’s Larsen C ice shelf could calve within “hours, days, or weeks,” researchers say.

Scientists monitoring the ice shelf report that from June 24 to June 27, the outer end of the iceberg started to accelerate to the fastest speeds ever recorded at this location — a development they say is a “notable departure from previous observations.”

As of May 31, the crack itself had just about 14km to go before the iceberg would break free. The crack has not lengthened in the past month, so the ice is still attached. But that ice has suddenly started to move far faster than it ever has: more than 10 metres per day.

Researchers can’t say when the rift will cause the ice to break off the shelf, but when it does calve, that will remove 10% of the Larsen C shelf. The 5200-square-km iceberg would then become the third largest in recorded history.

Larsen c ice hslef lenght may 31 2017 a luckman swansea university midas
The state of the Larsen C ice shelf’s rift through May 31, 2017. Courtesy MIDAS Project/A. Luckman, Swansea University

The increase in the iceberg’s movement speed is “another sign that the iceberg calving is imminent,” scientists from Swansea University in the UK wrote on the website for Project MIDAS, which is tracking the rift.

The researchers also warn that the break could destabilize the entire 50,000-square-km shelf and eventually cause it to disintegrate. This happened with the Larsen B ice shelf after a similar iceberg calved from there in 2002.

The Sentinel-1 satellite image data below illustrates the substantial change in ice speed from early June to late June.


The Project MIDAS team said on June 24 that the rift has been widening about two metres per day since the end of May, but there has been no observable change in the length of the crack since then.

When the iceberg does break free and sail into the Southern Ocean, it should not contribute to sea level rise, since it’s already on the water. But if the full Larsen C ice shelf collapses, the land-based glaciers that it is holding back could have a significant impact on sea level.

More details about the rift are available in our most recent feature about Antarctica’s Larsen C ice shelf

Dave Mosher contributed reporting to this post.

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