At its inner end there is an active glacier flowing from the massive Karpinsky Glacier in the northwest, as well other active glaciers stemming from the University Glacier in the southwest flow into the western shore of the fjord.
There is an active glacier flowing from the massive Karpinsky Glacier in the northwest, as well other active glaciers stemming from the University Glacier in the southwest flow into the western shore of the fjord. This is at its inner end.