In choosing the site of the hut on our Home Beach I had thought of the possibility of northerly winds bringing a swell, but had argued, first, that no heavy northerly swell had ever been recorded in the Sound; secondly, that a strong northerly wind was bound to bring pack which would damp the swell; thirdly, that the locality was excellently protected by the Barne Glacier; and finally, that the beach itself showed no signs of having been swept by the sea, the rock fragments composing it being completely angular.

When the hut was erected and I found that its foundation was only 11 feet above the level of the sea ice, I had a slight misgiving, but reassured myself again by reconsidering the circumstances that afforded shelter to the beach.

The fact that such question had been considered makes it easier to understand the attitude of mind that readmitted doubt in the face of phenomenal conditions.

The event has justified my original arguments, but I must confess a sense of having assumed security without