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, Etchū, 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
Kyūshū and Shikoku. The high mountains and the well watered valleys, the
abundance of forest trees, and wild and luxuriant vegetation,(11) give to
these islands an aspect of perennial verdure.
Public-domain text, read in full here on John Shaqi.
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