Most of the houses of Sitka are heavy log dwellings, some of which are clapboarded outside and smoothly finished within. In the winter season about a thousand Indians live here, the white population being composed of the usual government officials and agents, with a few storekeepers engaged in the fur traffic and general trade with the aborigines. Four or five hundred miners and prospectors gather here also in the winter, when it becomes too cold to prosecute their calling far inland, where the thermometer often falls to 20° below zero. Even this occasional extreme could be easily endured, and the work be little retarded, were suitable quarters provided. In midwinter daylight continues at Sitka for only six hours in the twenty-four, though by the first of June there is virtually no night at all; the stars take a vacation, while the evening and the morning twilight merge into day. The author had thought, heretofore, that the rainfall at Bergen, on the coast of Norway, exceeded that of any other spot he had visited, but here at Sitka “the rain, it raineth every day.” We have seen it rain harder in the tropics, but not often. The brief downpour, however, is so quickly followed by a flood of delicious sunshine that the contrast is a charming revelation. Still another effect is observable that, as rainy as it is, at certain seasons the atmosphere is still peculiarly dry. The writer was told that clothes would quickly dry under a shed during the heaviest rains. The fair weather is most likely to occur during the excursion season, so that the stranger is not apt to meet much annoyance in this respect while at the capital. The annual rainfall is recorded as being ninety inches upon this island, a degree of humidity which is attributed to the heated waters of the equatorial regions, which warm the whole coast-line of southern Alaska, insuring the mild winters it enjoys. Scientists tell us that the effect of this warm current is equivalent to twenty degrees of latitude, that is to say, the same products which are found in latitude 40° north on the Atlantic coast thrive in this region at 60° north, which is a little higher than the latitude of Sitka. This beneficent stream, arising off the coast of southern California, crosses the Pacific south of the Sandwich Islands, and on the coast of Asia turns northward in a grand sweep, striking the shores of America, and returning finally to its starting-point. “It is this,” says H. H. Bancroft, in his “History of the Pacific States,” “that clothes temperate isles in tropical verdure, makes the silkworm flourish far north of its rightful home, and sends joy to the heart of the hyperborean, even to him upon the Strait of Behring, and almost to the Arctic Sea.”