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Part 93

The Book of the Damned · Charles Fort — chapter 93 of 97 · ~1,028 words · public domain

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Its speed varied. Sometimes it seemed to outrun the train "considerably." At other times it seemed to fall behind. The mail-clerks watched until the town of Linville, Iowa, was reached. Behind the depot of this town, the light disappeared, and was not seen again. All this time there had been rain, but very little lightning, but Mr. Crotsenburg offers the explanation that it was "ball lightning."

The Editor of the Review disagrees. He thinks that the light may have been a reflection from the rain, or fog, or from leaves of trees, glistening with rain, or the train's light--not lights.

In the December number of the Review is a letter from Edward M. Boggs--that the light was a reflection, perhaps, from the glare--one light, this time--from the locomotive's fire-box, upon wet telegraph wires--an appearance that might not be striated by the wires, but consolidated into one rotundity--that it had seemed to oscillate with the undulations of the wires, and had seemed to change horizontal distance with the varying angles of reflection, and had seemed to advance or fall behind, when the train had rounded curves.

All of which is typical of the best of quasi-reasoning. It includes and assimilates diverse data: but it excludes that which will destroy it:

That, acceptably, the telegraph wires were alongside the track beyond, as well as leading to Linville.

Mr. Crotsenburg thinks of "ball lightning," which, though a sore bewilderment to most speculation, is usually supposed to be a correlate with the old system of thought: but his awareness of "something else" is expressed in other parts of his letters, when he says that he has something to tell that is "so strange that I should never have mentioned it, even to my friends, had it not been corroborated... so unreal that I hesitated to speak of it, fearing that it was some freak of the imagination."

Vast and black. The thing that was poised, like a crow over the moon.

Round and smooth. Cannon balls. Things that have fallen from the sky to this earth.

Our slippery brains.

Things like cannon balls have fallen, in storms, upon this earth. Like cannon balls are things that, in storms, have fallen to this earth.

Showers of blood.

Showers of blood.

Showers of blood.

Whatever it may have been, something like red-brick dust, or a red substance in a dried state, fell at Piedmont, Italy, Oct. 27, 1814 (Electric Magazine, 68-437). A red powder fell, in Switzerland, winter of 1867 (Pop. Sci. Rev., 10-112)--

That something, far from this earth, had bled--super-dragon that had rammed a comet--

Or that there are oceans of blood somewhere in the sky--substance that dries, and falls in a powder--wafts for ages in powdered form--that there is a vast area that will some day be known to aviators as the Desert of Blood. We attempt little of super-topography, at present, but Ocean of Blood, or Desert of Blood--or both--Italy is nearest to it--or to them.

I suspect that there were corpuscles in the substance that fell in Switzerland, but all that could be published in 1867 was that in this substance there was a high proportion of "variously shaped organic matter."

At Giessen, Germany, in 1821, according to the Report of the British Association, 5-2, fell a rain of a peach-red color. In this rain were flakes of a hyacinthine tint. It is said that this substance was organic: we are told that it was pyrrhine.

But distinctly enough, we are told of one red rain that it was of corpuscular composition--red snow, rather. It fell, March 12, 1876, near the Crystal Palace, London (Year Book of Facts, 1876-89; Nature, 13-414). As to the "red snow" of polar and mountainous regions, we have no opposition, because that "snow" has never been seen to fall from the sky: it is a growth of micro-organisms, or of a "protococcus," that spreads over snow that is on the ground. This time nothing is said of "sand from the Sahara." It is said of the red matter that fell in London, March 12, 1876, that it was composed of corpuscles--

Of course:

That they looked like "vegetable cells."

A note:

That nine days before had fallen the red substance--flesh--whatever it may have been--of Bath County, Kentucky.

I think that a super-egotist, vast, but not so vast as it had supposed, had refused to move to one side for a comet.

We summarize our general super-geographical expressions:

Gelatinous regions, sulphurous regions, frigid and tropical regions: a region that has been Source of Life relatively to this earth: regions wherein there is density so great that things from them, entering this earth's thin atmosphere, explode.

We have had a datum of explosive hailstones. We now have support to the acceptance that they had been formed in a medium far denser than air of this earth at sea-level. In the Popular Science News, 22-38, is an account of ice that had been formed, under great pressure, in the laboratory of the University of Virginia. When released and brought into contact with ordinary air, this ice exploded.

And again the flesh-like substance that fell in Kentucky: its flake-like formation. Here is a phenomenon that is familiar to us: it suggests flattening, under pressure. But the extraordinary inference is--pressure not equal on all sides. In the Annual Record of Science, 1873-350, it is said that, in 1873, after a heavy thunderstorm in Louisiana, a tremendous number of fish scales were found, for a distance of forty miles, along the banks of the Mississippi River: bushels of them picked up in single places: large scales that were said to be of the gar fish, a fish that weighs from five to fifty pounds. It seems impossible to accept this identification: one thinks of a substance that had been pressed into flakes or scales. And round hailstones with wide thin margins of ice irregularly around them--still, such hailstones seem to me more like things that had been stationary: had been held in a field of thin ice. In the Illustrated London News, 34-546, are drawings of hailstones so margined, as if they had been held in a sheet of ice.

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