he stream into which we have now passed is, literally, an immense salt-water river in the sea. Coming out of the Gulf of Mexico, it has brought the temperature of the tropics, all the way to the Banks of Newfoundland, in the latitude of 50° north, and it has run this distance between banks, or walls of cold water, on either side, parting with very little of its warmth, by the way. When it is recollected that this salt-water river in the sea is about three thousand times larger than the Mississippi River, that is to say, that it brings out of the Gulf of Mexico, three thousand times as much water, as that river empties into it, and that all this great body of water is carried up into the hyperborean regions of Newfoundland, at a temperature, even in mid-winter, ranging from 73 to 78 degrees, it will be seen at once what a powerful weather-breeder it must be. Accordingly, no port of the world is more stormy than the Gulf Stream, off the north-eastern coast of the United States, and the