HUDSON BAY.
Squalls of snow delayed us until the afternoon of the 13th, when we steamed westward along the north side of Digges islands. A bear was seen climbing over the cliffs, and a boat was lowered in chase, but the animal escaped. In the evening, the course was changed to northward, up Fox channel. At daylight the next morning ice was met with some ten miles from Leyson point. Steaming slowly through it, Seahorse point, on Southampton island, was reached at noon, and a landing was made with the launch. During the absence of the launch, the ship was sent out into the ice to the northeast, in order to examine its condition. It was found to be in large cakes of heavy rafted ice, too solid to penetrate at such a late date.
Walrus in Smith Sound.
Seahorse point is at the junction of the granites and gneisses with the Silurian limestones. There is here a marked difference between the southern limestone area and the northern country, underlain by the crystalline rocks, with its typical long, low, rounded hills, lying in roughly parallel ridges, and separated by wide shallow valleys, dotted with lakes and ponds, or filled with coarse boulder clay, with boulders scattered in bewildering profusion everywhere. This land, although high by contrast with the limestone country, seldom reaches an elevation of 500 feet, and that only far inland. There is one conspicuous peak, which rises like a great sugar loaf, far inland, its snow-capped summit of the lightest blue.
The limestone country occupies all the southern part of this great island, and also underlies the large islands of Coats and Mansfield farther to the south. The same physical characteristics prevail wherever the limestone is found. The low shores are bounded by gradually deepening water, broken by dangerous reefs that extend several miles from the land. The country rises very slowly inland, from the shores, in a succession of low, broad terraces, each a few feet higher than the one in front. These terraces are covered to a depth of several feet by broken limestone, which affords perfect drainage, and in consequence the surface is so dry that it will not even support a covering of the hardy Arctic plants. This absence of vegetation leaves the monotonous light-yellow shingle quite unrelieved by any dash of other colour, and the general view is one of dry desolation, much worse than that of the hilly country. The limestone region never reaches an elevation of one hundred feet within walking distance of the shore.
The ship lay-to during the night, among scattered pans of ice, about five miles from the land, and in forty fathoms of water. Late in the evening two walruses were killed on ice pans close to the ship.
A return to the southward was made at daylight, and the ice was finally left after passing Leyson point. During the passage through the ice, in the early morning, hundreds of walrus were seen asleep on the floating pans, and were left undisturbed. Skirting the low shores of the so-called Bell island, Evans strait was entered, and, late in the afternoon, we passed close to Walrus island in Fisher strait. This island is composed of crystalline rocks, and although not very high, it is conspicuous in contrast to the low shores on both sides of the strait. The island is much smaller than shown on the chart, and is only one island, not two, as marked there.
While passing through Evans and Fisher straits, soundings were taken every five miles. The bottom was found to be very even, and covered with fine sand or limestone debris. During the day the low shores of Southampton were in sight, without any feature sufficiently marked to afford a triangulation point.
The absence of ice in any part of Fisher strait led to the belief that no channel existed between Bell island and Southampton. This has since been confirmed by the captains of the Era and Active, both having narrowly escaped trouble in trying to pass through this supposed channel, which, if it does exist, is very shallow and narrow, even at high tide, and is so obstructed with shoals as to be absolutely dangerous.