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After a time the waves broke into what is called a "choppy sea;" the[Pg 315] wind was so great that their crests were blown away before they could rise to any height worthy of notice. Mariners say that in a severe typhoon the ocean is quite smooth, owing to the inability of the waves to form against the irresistible force of the wind. It is fortunate for them that such is the case, as they could not possibly survive the combined action of the cyclone and the great waves together.His voice trailed away and ended in a soft, tinkling sound, like sheep bells heard in the distance. During the long pause that followed Arthur had time to recall that sense of pity for this grotesque being which had accompanied his first impression of him; but now his feeling swelled into an infinite compassion, and with it there came to him a fierce questioning fever.
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"There is a curious story in connection with it. In 1816 a ship, the Canton, sailed from Sitka, and was supposed to have been lost at sea, as she never reached her destination. Fifty years later this island was discovered, and upon it was part of the wreck of the Canton. There were traces of the huts which were built by the crew during their stay, and it was evident that they constructed a smaller vessel from the fragments of the wreck, and sailed away in it."His lodgings were situated at the lower end of the town. The accommodation consisted[Pg 64] of a small bedroom, which he shared with a fellow clerk, and a place at table with the other inmates of the house. The street was very dirty, and Mrs. Flack's house alone presented some sign of decency and respectability. It was a two-storied red brick cottage. There was no front garden, and you entered directly into a living room through a door, upon which a brass plate was fixed that bore the following announcement:This part of Japan, and, in fact, the whole of Japan, has a good deal of volcanic fire pent up beneath it. Earthquakes are of frequent occurrence, and sometimes they are very destructive; whole towns have been destroyed by them, and as for the little ones that do no material damage, but simply give things a general shaking-up, they are so frequent as to be hardly noticeable. That there is an underground relation between the disturbances in different parts of the country is evident, and the tradition is that at the time of the last eruption of Fusiyama the ground rose considerably in the vicinity of the mountain, while there was a corresponding depression of the earth near Kioto, on the other side of the island. Occasionally there are slight rumblings in the interior of Fusiyama, but none of them are serious enough to excite any alarm.
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