Yes that coal ship did make the trip, but in the dangerous area at the top end of Peel Sound it was under icebreaker escort. If it had been required to make its own track and impact the big floes of Old ice as per the attached Ice chart, I doubt it would have been dent-free. Note that in several patches around the entrance to Peel Sound (areas L,I) as well as down in central Peel sound (area N) there are big floes of Old ice mixed into the ice cover. These are notoriously hard to detect in a dynamic ice cover, are thick and hard, and for any cruise ship (or coal ship) that hits them un-knowingly (foreign-going vessel with inexperienced crew), damage is a distinct possibility.
In this area (and to the north) a warm summer cleared out the First-year Fast Ice early, and allowed a "conduit" of Old Ice from the Arctic Ocean to feed down into Barrow Strait through Byam Martin channel. If warm summers continue, this mechanism is likely to feed progressively more Old Ice to this "choke point" in the Northwest Passage.