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 continuous, and pursued his journey far enough to see the open sea beyond, thus proving the existence of a passage at this point, though it was then, and probably ever will be, closed by an insurmountable barrier of ice. Besides this result of his endeavors, the position of Cockburn Island, and indeed of all the lands adjacent to Igloolik, was ascertained, and correctly laid down on the map.

Besides the Esquimaux found at Igloolik, our friends had the society of the savages of Winter Island, who rejoined them shortly after their arrival. We are sorry that we cannot relate the adventures and observations of this winter, as they are extremely entertaining; but as they are not important in their nature, we trust to be excused for omitting them.

Igloolik is a low island, ten miles long and six broad, and exhibits the same appearance of sterility as the adjacent continent, excepting in places which have been inhabited by the natives. There, the accumulation of animal substances has produced a luxuriant vegetation. In some parts there are spots several hundred yards in extent, covered with bright green moss. The whole land seems to be composed of innumerable fragments of thin schistose limestone, some of which contain the impressions of fossil remains, while others present the cellular structure usually found in madreporite. The interior is almost an entire swamp; but there are rising grounds, which, with the remains of Esquimaux habitations upon them, are excellent landmarks.

East of Igloolik is a group of small islands called by Captain Parry Calthorpe Islands. Like almost all the land in this vicinity, they are low, but their geology differs from that of Igloolik, and resembles that of Winter Island, being composed of gneiss. Two of this group, however, are high and rugged. From the top of one of these there is a view of the adjacent shores.

The entrance of the Strait of the Fury and Hecla is about three miles wide, and is formed by two projecting headlands between which the tide rushes with great velocity. The south shore is high, but of gradual ascent, perfectly smooth and composed of beautifully variegateds and-stone. Beyond the entrance the land is bold and mountainous. Captain Parry, who it will be remembered explored the southern shore of the Strait, states the hills to consist of gray gneiss and red granite, rising, in some instances, a thousand feet above the level of the sea. In some places he saw slate, and in others sand-stone. He has left no positive data, by which we may determine the length of this Strait; but as he was rather more than a day in accomplishing the distance on foot, by a circuitous route, we may conclude that it does not exceed fifteen or twenty miles. From the point where his journey terminated he saw a continuous sea to the westward, open and unobstructed save by ice and by one small island.

There are several islands in the Strait of the Fury and Hecla. On one of these (Liddon Island) abundance of beautifully veined clay iron-stone was found. The other minerals were asbestos, crystals of carbonate of lime, and a great variety of sand-stone, of which the island is formed.

Amherst Island is flat, and on the northern part is formed of black slate, with strong indications of coal. This part of the island is utterly bare of vegetation. In a low cliff of black and rugged slate there is a beautiful and romantic grotto. The water oozing through the sides and roof, has formed the most brilliant stalactites, which form a splendid contrast with the shady part of the ebon grotto behind. The other part of the