I'm intrigued by some rather strange valleys on the northern flank of Nordvestfjord in East Greenland, in Nathorsts Land. Two of then runn approx NE - SW, and the largest channel (the southernmost one) runs approx E -W. The northern channel, just to the south of the puramidal peak called Trianglen, has a prominent north-facing wall and is not very deep -- maybe 200m - 300m. It is may be 2 km long. The widdle channel is about 5 km long, and has a depth of c 700m. And the southern channel, which has an elongated lake on its floor, is about 8 km long.
These channels all carry signs of intensive glacial erosion and aerial scouring -- and glacial diffluence has clearly operated at some time -- but the channels do not obviously connect a glacier catchment with a discharge route, and I therefore speculate that at certain times during the Quaternary, during phases of catastrophic glacier melting, they may have been cut and used by huge volumes of meltwater.
I haven't found any references to these channels in the literature, and I will need to do some more research............
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