least for the present year, dependent upon an open season, and my most sanguine anticipations did not equal the apparent reality.
In order that the reader may appreciate, in some measure, the satisfaction which I took in the prospect that opened before me, it is necessary that I should here pause to give a general description of the region we were about to traverse, and an explanation of the physical conditions which made this portion of the Greenland waters of such conspicuous importance in the destinies of our voyage.
MELVILLE BAY. The shores of Melville Bay, as laid down on the maps, appear as a simple curved line of the Greenland coast; but the Melville Bay of the geographer comprehends much less than that of the mariner. The whalers have long called by that name the expansion of Baffin Bay which begins at the south with the "middle ice," and terminates at the north with the "North Water." The North Water is sometimes reached near Cape York, in latitude 76°, but more frequently higher up; and the "middle ice," which is more generally known as "the pack," sometimes stretches down to the Arctic Circle. This pack is made up of drifting ice-floes, varying in extent from feet to miles, and in thickness from inches to fathoms. These masses are sometimes pressed close together, having but little or no open space between them; and sometimes they are widely separated, depending upon the conditions of the wind and tide. They are always more or less in motion, drifting to the north, south, east, or west, with the winds and currents. The penetration of this barrier is usually an undertaking of weeks or months, and is ordinarily attended with much risk.
