The snowfall during the winter is comparatively small. There is probably not more than a foot of snow on a level anywhere on the land, though it is extremely difficult to measure or estimate, as it is so fine and dry that it is easily moved by the wind and is constantly in motion, forming deep, heavy, hard drifts under all the banks, while many exposed places, especially the top of the sand beach, are swept entirely clean. The snow begins to soften and melt about the first week in April, but goes off very slowly, so that the ground is not wholly bare before the middle or end of June. The grass, however, begins to turn green early in June, and a few flowers are seen in blossom as early as June 7 or 8. Rain begins to fall as early as April, but cold, snowy days are not uncommon later than that date. There is a good deal of clear, calm weather during the winter, and extremely low temperatures are seldom accompanied by high wind. Violent storms are not uncommon, however, especially in November, during the latter part of January, and in February. One gale from the south and southwest, which occurred January 22, 1882, reached a velocity of 100 miles an hour. The most agreeable season of the year is between the middle of May and the end of July, when the sea opens. After this there is much foggy and cloudy weather. Fresh-water ponds begin to freeze about the last week in September, and by the first or second week in October everything is sufficiently frozen for the natives to travel with sledges to fish through the ice of the inland rivers. Melting begins with the thawing of the snow, but the larger ponds are not clear of ice till the middle or end of July. The sea in most seasons is permanently closed by freezing and the moving in of heavy ice fields from about the middle of October to the end of July. The heavy ice in ordinary seasons does not move very far from the shore, while the sea is more or less encumbered with floating masses all summer. These usually ground on a bar which runs from the Seahorse Islands along the shore parallel to it and about 1,000 yards distant, forming a “barrier” or “land-floe” of high, broken hummocks, inshore of which the sea freezes over smooth and undisturbed by the pressure of the outer pack.