The Loss of the S.S. Titanic: Its Story and Its Lessons, by One of the Survivors

Once clear of the berg, we could read the Cunarder’s name—CARPATHIA—a name we are not likely ever to forget. We shall see her sometimes, perhaps, in the shipping lists,—as I have done already once when she left Genoa on her return voyage,—and the way her lights climbed up over the horizon in the darkness, the way she swung and showed her lighted portholes, and the moment when we read her name on her side will all come back in a flash; we shall live again the scene of rescue, and feel the same thrill of gratitude for all she brought us that night.

We rowed up to her about 4.30, and sheltering on the port side from the swell, held on by two ropes at the stern and bow. Women went up the side first, climbing rope ladders with a noose round their shoulders to help their ascent; men passengers scrambled next, and the crew last of all. The baby went up in a bag with the opening tied up: it had been quite well all the time, and never suffered any ill effects from its cold journey in the night. We set foot on deck with very thankful hearts, grateful beyond the possibility of adequate expression to feel a solid ship beneath us once more.

CHAPTER VI The Sinking of the Titanic Seen from Her Deck

The two preceding chapters have been to a large extent the narrative of a single eyewitness and an account of the escape of one boat only from the Titanic’s side. It will be well now to return to the Titanic and reconstruct a more general and complete account from the experiences of many people in different parts of the ship. A considerable part of these experiences was related to the writer first hand by survivors, both on board the Carpathia and at other times, but some are derived from other sources which are probably as accurate as first-hand information. Other reports, which seemed at first sight to have been founded on the testimony of eyewitnesses, have been found on examination to have passed through several hands, and have therefore been rejected. The testimony even of eye-witnesses has in some cases been excluded when it seemed not to agree with direct evidence of a number of other witnesses or with what reasoned judgment considered probable in the circumstances. In this category are the reports of explosions before the Titanic sank, the breaking of the ship in two parts, the suicide of officers. It would be well to notice here that the Titanic was in her correct course, the southerly one, and in the position which prudence dictates as a safe one under the ordinary conditions at that time of the year: to be strictly accurate she was sixteen miles south of the regular summer route which all companies follow from January to August.

Perhaps the real history of the disaster should commence with the afternoon of Sunday, when Marconigrams were received by the Titanic from the ships ahead of her, warning her of the existence of icebergs. In connection with this must be taken the marked fall of temperature observed by everyone in the afternoon and evening of this day as well as the very low temperature of the water. These have generally been taken to indicate that without any possibility of doubt we were near an iceberg region, and the severest condemnation has been poured on the heads of the officers and captain for not having regard to these climatic conditions; but here caution is necessary. There can be little doubt now that the low temperature observed can be traced to the icebergs and ice-field subsequently encountered, but experienced sailors are aware that it might have been observed without any icebergs being near. The cold Labrador current sweeps down by Newfoundland across the track of Atlantic liners, but does not necessarily carry icebergs with it; cold winds blow from Greenland and Labrador and not always from icebergs and ice-fields. So that falls in temperature of sea and air are not prima facie evidence of the close proximity of icebergs. On the other hand, a single iceberg separated by many miles from its fellows might sink a ship, but certainly would not cause a drop in temperature either of the air or water. Then, as the Labrador current meets the warm Gulf Stream flowing from the Gulf of Mexico across to Europe, they do not necessarily intermingle, nor do they always run side by side or one on top of the other, but often interlaced, like the fingers of two hands. As a ship sails across this region the thermometer will record within a few miles temperatures of 34°, 58°, 35°, 59°, and so on.