The Nunatak Glacier originates at the eastern end of the Adolf Hoel Glacier, south of the area of the Jakob Kjøde Bjerg nunatak. Strindberg Land lies to the east and the northeastern end of Andrée Land on its western side.
It flows in a roughly northwest to southeast direction for about 20 km (12 mi) until its terminus at the head of the Geologfjord.[2] The Eyvind Fjeld Glacier flows beyond the northwestern end of the Nunatak Glacier, to the west of Jakob Kjøde Bjerg.[3]
Bibliography
A. K. Higgins, Jane A. Gilotti, M. Paul Smith (eds.), The Greenland Caledonides: Evolution of the Northeast Margin of Laurentia.