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mate of all parts over which the winds extend. The same monsoon blows over the eastern countries of the continent, but the insular character of Japan and the proximity of the warm current on both sides of the islands give to the winds which prevail a character which they do not possess on the continent. During the greater part of September the northern wind blows, which brings a colder temperature, condensing the moisture contained in the atmosphere. This month is therefore generally a rainy month. Gradually the atmosphere becomes more dry, and the beautiful autumn and early winter follow in course. The winter is very different in the different parts. On the east coast the temperature is very moderate. Even as far north as Tokyo the snow rarely falls to a depth of more than a few inches, and then rapidly melts away. Ice seldom forms to a thickness, even on protected waters, to permit skating. In all this region, however, snow covers the high mountains. On the west coast of the Main island the conditions are very different. The winds of the continent take up the moisture of the Japan sea, and carry it to the west coast, and then, coming in contact with high ranges of mountains which run down the middle of the island, impart their moisture in the form of rain in summer, and snow in winter. These circumstances produce extraordinary falls of snow on the west coast. This is particularly true of the provinces of Kaga, Noto, Etchu, Echigo, and even farther north, especially in the mountainous regions. In the northern part of these districts the snow is often as much as twenty feet deep during the winter months. The inhabitants are obliged to live in the second stories of their houses and often find it necessary to make steps from their houses out to the top of the snow. One effect of these deep snows is to cover up with a safe protection the shrubs and tender plants which would otherwise be exposed to the chilling winds of winter. By this means the tea-shrub and the camellia, which could not withstand the open winter winds, are protected so as to grow luxuriantly. The southern islands are materially warmer than the Main island. The tropical current together with the warm sunshine due to their low latitude, immerses them in a moist and warm atmosphere. Their productions are of a sub-tropical character. Cotton, rice, tobacco, sugar, sweet potatoes, oranges, yams, and other plants of a warm latitude, flourish in Kyushu and S
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