79N is a "tongue" of glacier around 50 miles long by 12.5 miles wide.
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It is the floating tip of the Northeast Greenland Ice Stream, where it flows off the edge of the land and onto the sea. A northern offshoot from the stream, known as the Spalte Glacier, is the part that has broken off.
A gif showing the progressive disintegration of the Spalte Glacier between 2013 and 2020.Promice
The once-solid ice now floats in pieces. According to Prof Jason Box of GEUS, it will become a hotspot for the future warming of Greenland.
"What makes 79N so important is the way it's attached to the interior ice sheet, and that means that one day — if the climate warms as we expect — this region will probably become one of the major centres of action for the deglaciation of Greenland."
Scientists are connecting the event to climate change. Dr Jenny Turton, a researcher into the 79N glacier at the University of Erlangen-Nuremberg, said that the region's atmosphere has warmed by around 3 degrees Celsius (5.4 degrees Fahrenheit) since 1980.
There were record-breaking temperatures in the area in both 2019 and 2020, Dr Turton said.
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Since 1999, the 79N ice shelf has lost an area twice the size of Manhattan, according to GEUS.
Dr Turton said the warmer summers accelerate the melting, as run-off water from the ice sheet causes rivers and pools on the surface of the "tongue" of the glacier.
As they re-freeze in winter, they create additional pressure on the glacier. Warmer sea temperatures below the glacier also contribute to the effect, according to the BBC.
A zoomed-in detail (L) from the 79N glacier, marked up by Business Insider, showing the meltwater rivers and pools that speed up how it breaks upCopernicus Data/ESA/Sentinel-2B/PromiceGL/Business Insider
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