Report on the Dominion Government Expedition to Hudson Bay and the Arctic Islands on board the D.G.S. Neptune, 1903-1904

by A. P. Low

Midnight in Smith Sound.

Similar lanes of water, between large cakes of ice, afforded an easy passage from Mansfield to Digges islands. A great amount of ice was seen to the southward, apparently completely filling the channel between Mansfield and the mainland. To the northward some open water occurred, but the patches became smaller and smaller as Digges was approached, and finally ceased to the eastward of these islands, the southern part of the western end of Hudson strait being completely filled with ice.

A strong southerly wind had been blowing all day, and it was hoped that it had loosened the ice along the southern shore of the strait. The ship was taken under the land, but without success, so that after butting through the slowly closing ice all night, we were finally tightly beset in the early morning, about three miles from the eastern Digges island. The 21st was foggy, with snow flurries in the morning and showers in the afternoon; the ice remained tight about the ship all day, and she drifted eastward with the ice, passing Cape Wolstenholme, and in the evening being about five miles to the east of Erik cove. At that time considerable open water could be seen about five miles from the ship to the eastward, with a few narrow lanes in the rear, and other small openings to the northward, where the dark sky showed considerable open water beyond our view.

HUDSON STRAIT.

Persistent ramming forced the ship through about five miles of ice on the morning of the 22nd, when she was again tightly beset until the evening, at that time being about twenty-five miles to the eastward of Cape Wolstenholme, this distance having been made by the drift of the ice. The ice slackened again at eight o’clock in the evening, when after an hour’s heavy work we got into a lead of open water under the land, and continued at full speed all night, steaming east in a lane from two to four miles wide.

At five o’clock next morning we were off Deception bay and the western end of Charles island. The bold coast along which we had been passing all night now became less abrupt, and this change was accompanied by shallower water in the sea fronting it, so that when seven miles from the mouth of the bay, soundings taken at the edge of the ice only gave twelve fathoms, with indications of an uneven bottom, where it would be dangerous to be caught in the ice if the wind should change and force it upon the land. The ship was turned into the ice, and in an hour had reached a place of safety. In the afternoon, with clearing weather, the ice opened, and not much difficulty was experienced in forcing between the loose pans, first towards the east end of Charles island and later more easterly, so that when the ice again closed we were about ten miles northeast of Cape Weggs.

During the night and following morning we continued to drift rapidly to the eastward. Before noon we were opposite the mouth of Douglas harbour, having made fully twenty miles of drift during that interval.

The ice began to slacken at ten o’clock, when we got under way, and forcing the ship towards the north at noon we were in open water, with a heavy northerly swell, which showed an open sea in that direction. Only a few small icebergs and broken pans of ice were seen during the remainder of the trip to Port Burwell, which we reached on the evening of the 25th, but in crossing Ungava bay the lower temperature and an ice-glint to the southward indicated some ice in the southern part of that bay.

The following summary of the condition and extent of the ice met with on the passage from Fullerton to Port Burwell may prove of interest and value. The northwestern part of Hudson bay was quite free of ice, and none to obstruct navigation was found in Fisher and Evans straits. Large quantities of ice were encountered between the mouth of Evans strait and Digges at the western end of Hudson strait, but without serious trouble safe passages were found through it, and there is no doubt that an ordinary unprotected iron steamship would have passed through it at that time without trouble or danger. This ice, evidently the product of the past winter, consisted chiefly, as has been mentioned, of large flat sheets that had only a short time previously broken from their original position, for there were no signs that it had been subjected to pressure or to the action of a swell. The edges of these large cakes had not been crushed, and many soft thin spots were seen which would disappear with the slightest pressure or swell. Along with the predominating flat ice was a considerable amount of rafted ice of the same character, and also of portions apparently subjected to pressure during the past winter. All the ice was comparatively light and thin, which led to the belief that it had come out of Fisher strait, and from the southward up the channel between Mansfield and the eastern mainland, the meeting of these streams producing the blockade at the western end of Hudson strait. Owing to its thinness and rotten character, the greater part of this ice would melt a few days after we passed it.