The Roosevelt Range is an up to high mountain range in Northern Peary Land, formed by alpine-type mountains. The topography of the mountains is deeply eroded, with sharp, jagged ridges and precipitous cliffs. The area of the range is uninhabited. Owing to a structural continuum in the mountains between Johannes V. Jensen Land in the east and Nansen Land in the west, American geologist William E. Davies called the wider range the "Nansen-Jensen Alps" in a work he published in 1972. The Roosevelt Range would be thus a subrange of a wider mountain chain with its westernmost foothills in Nansen Land, reaching all the way to Johannes V. Jensen Land in the east. The Roosevelt Range proper rises in Roosevelt Land in the west and stretches eastward across Gertrude Rask Land, north of a valley between the heads of the Harder Fjord in the west and the Frigg Fjord in the east. It extends eastwards in Johannes V. Jensen Land north of the Frederick E. Hyde Fjord beyond the Polar Corridor , a mountain pass connecting two glacial valleys running from North to South between the heads of Sands Fjord to the north and Frigg Fjord to the south. Its easternmost subranges almost reach the eastern end of northern Peary Land. The area near the Lincoln Sea coast, southwest of Cape Morris Jesup is known as Ulvebakkerne.
Peaks
Apart from its highest point Helvetia Tinde, not many peaks of the Roosevelt Range have been named. Other relevant mountains in the range are Paradisfjeld and Mary Peary Peaks', located east of the Polar Corridor in a roughly central position, as well as Birgit Koch Peaks' and Rink Mountain , a little further to the east.
Subranges
The H. H. Benedict Range ', highest point Stjernebannertinde, and the Daly Range ', both located at the eastern end in Johannes V. Jensen Land, are subranges of the Roosevelt Range.
Glaciers
The valleys between mountains are filled with glaciers or icefields, none of which are very large. In the same manner as other features in this range many glaciers are unnamed.
Thomas Glacier
Raven Glacier
A. Harmsworth Glacier
Modvind Glacier
Nord Glacier
Syd Glacier
Malcantone Glacier
Nysne Glacier
Sif Glacier
Borup Glacier
Moore Glacier
Ydun Glacier
Bertelsen Glacier
Geology
The Roosevelt Range forms the northern sub-region of the Innuitian orogeny. It is part of the belt Caledonian folding that extends eastward from north Ellesmere Island. The ages of rocks in the range area are from Precambrian to Upper Silurian, with low-grade marbles, psammites, sandstone, shales, quartzite and mudstones.