The terminus of Fridtjovbreen in 2009, nearly a decade after the surge, showing rapid recession through calving. A large sediment plume emanates from the terminus, and dead ice is stranded along the moraine-draped flanks of the bay. (MH) |
The terminus of Fridtjovbreen in 2009, nearly a decade after the surge, showing rapid recession through calving. A large sediment plume emanates from the terminus, and dead ice is stranded along the moraine-draped flanks of the bay. (MH) |