To the north the fjord has its mouth in the Lincoln Sea of the Arctic Ocean.

On the western Roosevelt Land side the fjord is under the influence of slow-moving glaciers discharging on both sides of Cape Kane that completely fill it and partially clog neighboring Conger Sund as well.

[4] The large Thomas Glacier discharges at the head of Hunt Fjord from the western end of the Roosevelt Range.

[5] The Raven Glacier discharges on the eastern side, closer to the mouth, south of Cape Washington.

[6] The western shore of the fjord is glaciated with dark pointed nunataks protruding between short valleys filled with glaciers.