But I realised when looking at the image that the next glacier to the west -- Borgbjerg Gletscher -- experienced a much bigger surge, probably at the same time, with a calving ice front out in the fjord. Also -- and this is extremely rare -- there is an extensive area of dead ice or ice-cored moraine very close to the shoreline, around 6 km from the present glacier edge. You can see the pockmark pattern of small meltwater pools. As with Löberen next door, the ice edge retreat post-surge is approx 8 km over approx 60 years.
If you look at the glaciers as they are today, they are covered with bright blue meltwater pools -- a characteristic of glaciers that are "healing" themselves following the drastic changes in ice surface elevation caused by a period of rapid ice flow.
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