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 and proved to be in Norton Sound, between Cape Tchaplin on the Asiatic and Cape Stephens on the American coast, but a hundred miles from either.

"We must give up all hope of making the land of the continent then!" said Mrs Barnett.

"Yes, madam," replied Hobson; "all hope of that is at an end; the current is carrying us with great rapidity out into the offing, and our only chance is, that we may pass within sight of a whaler,"

"Well, but," added Mrs Barnett, "if we cannot make the land of either continent, might not the current drive us on to one of the islands of Behring Sea?"

There was, in fact, a slight possibility that such a thing might happen, and all eagerly clutched at the hope, like a drowning man at a plank. There are plenty of islands in Behring Sea, St Lawrence, St Matthew, Nunivak, St Paul, George Island, &c. The wandering island was in fact at that moment not far from St Lawrence, which is of a considerable size, and surrounded with islets; and should it pass it without stopping, there was yet a hope that the cluster of the Aleutian Islands, bounding Behring Sea on the south, might arrest its course.

Yes! St Lawrence might be a harbour of refuge for the colonists, and if it failed them, St Matthew, and the group of islets of which it is the centre, would still be left. It would not do, however, to count upon the Aleutian Islands, which were more than eight hundred miles away, and which they might never reach. Long, long before they got so far, Victoria Island, worn away by the warm sea-waves, and melted by the rays of the sun, which was already in the sign of Gemini, would most likely have sunk to the bottom of the ocean.

There is, however, no fixed point beyond which floating ice does not advance. It approaches nearer to the equator in the southern than in the northern hemisphere. Icebergs have been seen off the Cape of Good Hope, at about thirty-six degrees south latitude, but those which come down from the Arctic Ocean have never passed forty degrees north latitude. The weather conditions, which are of course variable, determine the exact locality where ice will melt; in severe and prolonged winters it remains solid in comparatively low latitudes, and vice versa in early springs.

Now the warm season of 1861 had set in very early, and this would hasten the dissolution of Victoria Island. The waters of