In latitude 51 deg. 33' south, and longitude 321 deg. 00' east, the wind seemed set in at south-west, and blew a fresh steady gale, frequently attended with showers of snow or hail; the variation of the compass decreased fast, as will appear in the table annexed. On the 16th the wind shifted suddenly to the north-west quarter, and blew a steady gale. On the 19th, it blew very strong from west-north-west, with hazy weather, and frequent showers of rain, which again changed the wind to the south-west quarter, and the weather, as usual upon those changes, became fair and pleasant. We now seemed to have got out from among the ice-islands, with which, from South Georgia to the latitude of 46 deg. south, this ocean seems at this season of the year to be overspread. In latitude 44 deg. 00' south, we saw the last piece of ice, and in the whole, we had been twenty-eight days among the ice, and sailed a distance of 800 leagues. We had run for several days together, at the rate of from 50 to 60 leagues in the 24 hours, in a north-east direction; and had passed through a lane or street, if it may be so called, of ice-islands, the whole of that distance: in general they were from the size of a country church, to the magnitude of one, two and three miles in circumference, and proportionably high. Were it not that at this season of the year we had in such high latitudes very short nights, and scarcely an hour which could be called dark; it would certainly be attended with considerable danger to run in the night, the ice islands were in such vast numbers; indeed, we seldom sailed more than three or four miles, without having several upon each beam. I think the direction, in which those pieces of ice seemed to have been driven, is a strong proof of the prevalence of south-west winds in this part of the ocean. It is highly probable that they had been formed upon the coast of South Georgia and Sandwich Land, and separated from the ground early in the spring, or probably in a gale of wind during the winter. Many of them were half black, apparently with earth from the land to which they had adhered, or else, with mud from the bottom on which they had lain: for it is well known, that ice-islands, after having been driven about at sea for a length of time, become so light and spungy in that part which has been immersed in the water, that the upper part becomes heavier, and thereby they frequently overset, and may, by such a change, show some part of the ground on which they had rested. Others had large and distinct portions of them thoroughly tinged with a beautiful sea-green, or bright verdigrease colour.