"Thursday, February 22d. The net-line has pointed west all day till now, afternoon, when it is pointing straight up and down, and we are presumably lying still. The wind slackened to-day till it was quite calm in the afternoon. Then there came a faint breeze from the southwest and from the west, and this evening the long-dreaded northwester has come at last. At 9 P.M. it is blowing pretty hard from N.N.W. An observation of Capella taken in the afternoon would seem to show that we are in any case not farther north than 80° 11' and this after almost four days' south wind. Whatever can be the meaning of this? Is there dead-water under the ice, keeping it from going either forward or backward? The ice to starboard cracked yesterday, away beyond the bear-trap. The thickness of the solid floe was 11 1/2 feet (3.45 metres), but, besides this, other ice was packed on to it below. Where it was broken across, the floe showed a marked stratified formation, recalling the stratification of a glacier. Even the darker and dirtier strata were there, the color in this case produced by the brownish-red organisms that inhabit the water, specimens of which I found at an earlier date. In several places the strata were bent and broken, exactly in the same manner as the geological strata forming the earth's crust. This was evidently the result of the horizontal pressure in the ice at the time of packing. It was especially noticeable at one place, near a huge mound formed during the last pressure. Here the strata looked very much as they are represented in the annexed drawing. [46] It was extraordinary too to see how this floe of over three yards in thickness was bent into great waves without breaking. This was clearly done by pressure, and was specially noticeable, more particularly near the pressure-ridges, which had forced the floe down so that its upper surface lay even with the water-line, while at other places it was a good half-yard above it, in these last cases thrust up by ice pressed in below. It all shows how extremely plastic these floes are, in spite of the cold; the temperature of the ice near the surface must have been from 4° Fahr. to 22° Fahr. below zero (-20° to -30° C.) at the time of these pressures. In many places the bending had been too violent, and the floe had cracked. The cracks were often covered with loose ice, so that one could easily enough fall into them, just as in crossing a dangerous glacier. "Saturday, February 24th. Observations to-day show us to be in 79° 54' north latitude, 132° 57' east longitude. Strange that we should have come so far south when the north or northwest wind only blew for twenty-four hours.