I found another striking image of the bench on the north side of Nordvestfjord while going through my vast air photo collection. It shows the feature with great clarity -- looking from NW towards SE. In the far distance we can see Scoresbysund and Jameson Land.
The bench is referred to as a relict planation feature -- and labelled as part of the LPS or lower planation surface by Bonow and Japsen. If the dissected plateau edge coincides with the outcrop of a basaltic layer, we can argue for some geological control. Bonow and Japsen argue that there is an erosion surface that passes beneath the basalt -- they refer to this as an "etchplain". They claim thast the feature must have formed later than mid-Miocene..........
But the extent of ice moulding is also very striking. All in all, this has to be a composite feature owing its origin to multiple changes of climate over a vast stretch of geological time.
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