It had reached a point somewhere to the southwest, and not very far from Jamaica, by September 2d. The morning of September 3d found it about 175 miles south of the middle of Cuba. It had moved northwestward to latitude 21 degrees and longitude 81 degrees by September 4th. Up to this time the storm had not developed any destructive force but had caused heavy rains, particularly at Santiago, Cuba, where 12.58 inches of rain fell in twenty-four hours.

OMINOUS PROGRESS OF THE STORM.

On the morning of the fifth, the storm centre had passed over Cuba and had become central between Havana and Key West. High winds occurred over Cuba during the night of the fourth. By the morning of the sixth the storm centre was a short distance northwest of Key West, Fla., and the high winds had commenced over Southern Florida, forty-eight miles an hour from the east being reported from Jupiter, and forty miles from the N. E. from Key West. At this time it became a question as to whether the storm would recurve and pass up along the Atlantic coast, a most natural presumption judging from the barometric conditions over the eastern portion of the United States, or whether it would continue northwesterly over the Gulf of Mexico.

Advisory messages were sent as early as September 1st to Key West and the Bahama Islands, giving warning of the approach of the storm and advising caution to all shipping. The warnings were supplemented by others on the second, third, and fourth, giving more detailed information, and were gradually extended along the Gulf coast as far as Galveston and the Atlantic coast to Norfolk.

On the afternoon of the fourth the first storm warnings were issued to all ports in Florida from Cedar Keys to Jupiter. On the fifth they were extended to Hatteras, and advisory messages issued along the coast as far as Boston. Hurricane warnings were also ordered displayed on the night of the fifth from Cedar Keys to Savannah. On the fifth storm warnings were also ordered displayed on the Gulf coast from Pensacola, Fla., to Port Eads, La. During the sixth barometric conditions over the eastern portion of the United States so far changed as to prevent the movement of the storm along the Atlantic coast, and it therefore continued northwest over the Gulf of Mexico.

On the morning of the seventh it was apparently central south of the Louisiana coast, about longitude 28, latitude 89. At this time storm signals were ordered up on the North Texas coast, and during the day were extended along the entire coast. On the morning of the eighth the storm was nearing the Texas coast, and was apparently central at about latitude 28, longitude 94. The last report received from Galveston, dated 3.40 P. M., September 8, showed a barometric pressure of 29.22 inches, with a wind of forty-two miles an hour, northeast, indicating that the centre of the storm was quite close to that city.

ALWAYS IN DANGER DURING A HURRICANE.

At this time the heavy sea from the southeast was constantly rising and already covered the streets of about half the city. Up to Sunday morning no reports were received from southern Texas, but the barometer at Fort Worth gave some indications that the storm was passing into the southern portion of the State. An observation taken at San Antonio at 11 o’clock, but not received until half-past five, indicated that the centre of the storm had passed a short distance east of the place, and had then turned in the northward.

Situated as Galveston is, with much of the shore but a few feet above the mean high water, there is so scant a margin of safety that, as was the case on the South Carolina Sea Islands on August 27, 1893, and among the bayous of Louisiana in October of the same year, any abnormal tide means death and destruction. Sabine Pass is a mere sand spit, and Galveston Island itself is but a few feet above the ocean level at the best, and is but three feet above high tide in many places. As the great storm wave raised by the cyclonic winds of the average hurricane may easily have a crest of from eight to nine feet, for a city such as Galveston this would be most ominous.

Such a fate as an inundation during the prevalence of a hurricane has been forecast for the island city, whose population according to the new census is 37,789, many of whom live under conditions that invite loss of life in case of a tidal overflow. And yet, though such a disaster has been foreseen and forecast, the inertia of one’s adherence to normal life and duties is such that even in the face of specific warning it is not likely any number would flee to the mainland. On September 8th, for instance, the Weather Bureau, which had not lost track of the storm, very correctly pointed out that the hurricane was moving northwestward slowly, towards the Texas coast, Port Eads, La., giving a wind velocity of fifty-six miles an hour. Storm warnings were ordered for the eastern Texas and middle Gulf region, and high winds were specifically forecast for the coast of eastern Texas. More the Bureau could not do, but it looks as if its warnings were in vain.