The narrowness and openness of the ice at this season, between the parallels of 73° and 74°, when compared with its extent and closeness about the same time the preceding year, was a decided confirmation, if any were wanting, that the summer of 1824 was extremely unfavourable for penetrating to the westward about the usual latitudes. How it had proved elsewhere we could not of course conjecture, till, on the 8th, being in latitude 71° 55′, longitude 60° 30′, and close to the margin of the ice, we fell in with the _Alfred_, _Ellison_, and _Elizabeth_, whalers of Hull, all running to the northward, even at this season, to look for whales. From them we learned that the _Ellison_ was one of the two ships we saw, when beset in the “pack” on the 18th July, 1824; and that they were then, as we had conjectured, on their return from the northward, in consequence of having failed in effecting a passage to the westward. The master of the _Ellison_ informed us that, after continuing their course along the margin of the ice to the southward, they at length passed through it to the western land without any difficulty, in the latitude of 68° to 69°. Many other ships had also crossed about the same parallels, even in three or four days; but none, it seemed, had succeeded in doing so, as usual, to the northward. Thus it plainly appeared (and I need not hesitate to confess that to me the information was satisfactory) that our bad success in pushing across the ice in Baffin’s Bay in 1824, had been caused by circumstances neither to be foreseen nor controlled; namely, by a particular position of the ice, which, according to the best information I have been able to collect, has never before occurred during the only six years that it has been customary for the whalers to cross this ice at all, and which, therefore, in all probability, will seldom occur again. If we seek for a cause for the ice thus hanging with more than ordinary tenacity to the northward, the comparative coldness of the season indicated by our meteorological observations may perhaps be considered sufficient to furnish it. For as the annual clearing of the northern parts of Baffin’s Bay depends entirely on the time of the disruption of the ice, and the rate at which it is afterwards drifted to the southward by the excess of northerly winds, any circumstance tending to retain it in the bays and inlets to a later period than usual, and subsequently to hold it together in large floes, which drive more slowly than smaller masses, would undoubtedly produce the effect in question. There is, at all events, one useful practical inference to be drawn from what has been stated, which is that, though perhaps in a considerable majority of years a northern latitude may prove the most favourable for crossing in, yet seasons will sometimes intervene in which it will be a matter of great uncertainty whereabouts to make the attempt with the best hope of success.