as a consequence they got frostbitten. There was lively cheering when they reappeared in this condition, such is the sympathy which is here displayed for affliction; but with Wilson much of the amusement arises from his peculiarly scant headgear and the confessed jealousy of those of us who cannot face the weather with so little face protection.
The wind dropped at night.
Sunday, May 21.—Observed as usual. It blew from the north in the morning. Had an idea to go to Cape Royds this evening, but it was reported that the open water reached to the Barne Glacier, and last night my own observation seemed to confirm this.
This afternoon I started out for the open water. I found the ice solid off the Barne Glacier tongue, but always ahead of me a dark horizon as though I was within a very short distance of its edge. I held on with this appearance still holding up to C. Barne itself and then past that Cape and half way between it and C. Royds. This was far enough to make it evident that the ice was continuous to C. Royds, and has been so for a long time. Under these circumstances the continual appearance of open water to the north is most extraordinary and quite inexplicable.
Have had some very interesting discussions with Wilson, Wright, and Taylor on the ice formations to the west. How to account for the marine organisms found on the weathered glacier ice north of the Koettlitz Glacier? We have been elaborating a theory under which this ice had once a negative buoyancy due to the morainic material
