But Hindostan has far greater horrors to report. A terrible flood in 1887 was driven by the cyclone over the Ganges delta. The victims numbered many thousands: exact figures not at hand. But in 1876, a cyclone swept the Backergunge district, and rolled in a storm wave over the eastern edge of the fertile delta, covering it with from ten to fifty feet of water. When the storm had subsided, it was found that more than one hundred thousand people had perished! Finally, a great cyclone in 1737, October 11-12, swept the Ganges delta with a wave thirty feet deep on the land. Three hundred thousand people perished in this storm! The mind can not grasp the appalling magnitude of such a disaster. These cases are the most destructive cyclones on record, and in each case the destruction is due largely to the character of the region traversed, though the winds of Bengal are not surpassed in violence by those of any country in the world. Were the harbor an open seaport, instead of a large river, no ship could live through such a storm. Other regions in the east suffer much from tempests. The whole Malay archipelago, with the Moluccas and Philippines, are visited quite as frequently as the coasts of Hindostan. A cyclone that swept the Philippine Islands, November 6, 1885, destroyed ten thousand people, and millions of dollars worth of property. The same character of storms is frequently met with in the Japan and China seas, where it is known as the “typhoon,” our Anglicised spelling of the Chinese title, “tei-fun.” With one example of the power of this storm, this chapter must close. In the narrative of Commander Hall, of the British Navy, is found this description of a typhoon that occurred at Hong Kong, July 21-22, 1841: “For days previously large black clouds appeared to [Illustration: COAST OF INDIA SUBMERGED BY A STORM.]