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Bentarasko Benta Section 04
Page 08
In 1891 a teacher in the Kumamoto Boys' School gave expression to the thought in a public address that, as all mankind are brothers, the school should stand for the principle of universal brotherhood and universal goodwill to men. This expression of universalism was so obnoxious to the patriotic spirit of so large a number of the people of Kumamoto Ken, or Province, that the governor required the school to dismiss that teacher. There is to-day a strong party in Japan which makes "Japanism" their cry; they denounce all expressions of universal good-will as proofs of deficiency of patriotism. There are not wanting those who see through the shallowness of such views and who vigorously oppose and condemn such narrow patriotism. Yet the fact that it exists to-day with such force must be noted and its natural explanation, too, must not be forgotten. It is an indication of self-conscious nationality.
As the river seemed to describe a big loop, I had left it three days before, seeing plainly by the conformation of the country that we should strike it again sooner or later. We were marching once more by compass. My men, who had no faith whatever in the magnetic needle, were again almost paralysed with fear that we might not encounter the stream again. A thousand times a day they accused me of foolishness in leaving the river, as they said it would have been better to follow its tortuous course--notwithstanding the trouble we had in following it, owing to the dense vegetation near the water--rather than strike once more across country. They were beginning to lose heart altogether, when I told them I could see by the vegetation that we were once more near the water. Anybody accustomed as I am to marching through the forest could tell easily by the appearance of the vegetation some miles before actually getting to a stream.
Owing to many natural causes the river may, after a while, cease to flow, leaving enlarged portions of its channel behind as a succession of chambers in a cave. But water would still come trickling in from the tops and sides, and be continuously dripping to the floor, where it speedily evaporates. When such is the case it leaves behind it the limestone it held in solution. So, in process of time, if the deposition is undisturbed, there will be formed over the floor of the cave a more or less continuous layer of limestone matter known as stalagmite. The same formations on the top and sides of the cave are called stalactites. In places where the drip is continuous the stalactite gradually assumes the shape of an immense icicle; while the stalagmite on the floor of the cave, underneath the drip, rises in a columnar mass to meet the descending stalactite. A union of these is not uncommon, and, we have pillars and columns presenting the strange, fantastic appearance on which tourists delight to dwell in their notes of travel.
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