Authors: Charles Fort
I think, myself, that there was one approximately great, wise astronomer. He was Tycho Brahé. For many years, he would not describe what he saw in the sky, because he considered it beneath his dignity to write a book. The undignified, or more or less literary, or sometimes altogether too literary, astronomers, who do write books, uncompromisingly say that when a luminous object is said to have moved to greater degree than could be considered illusory, in a local sky of this earth, it is a fire balloon. It is not possible to find in the writings of astronomers who so explain, mention of the object that was seen by Coggia, night of Aug. 1, 1871. It seems that this thing was not far away, and did appear only in a local sky of this earth, and if it did come from outer space, how it could have “boarded” this earth, if this earth moves at a rate of nineteen miles a second, or one mile a second, is so hard to explain that why Proctor and Hind, with their passionate itch for explaining, never took the matter up, I don’t know. Upon Aug. 1, 1871, an unknown luminous object was seen in the sky of Marseilles, by Coggia
(Comptes Rendus,
73-398). According to description, it was a magnificent red object. It appeared at 10:43 p.m. and moved eastward, slowly, until 10:52:30. It stopped—moved northward, and again, at 10:59:30, was stationary. It turned eastward again, and, at 11:3:20, disappeared, or fell behind the horizon. Upon this night Venus was within three weeks of primary greatest brilliance, inferior conjunction occurring upon Sept. 25, 1871.
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One repeating mystery—the mystery of the local sky.
How, if this earth be a moving earth, could anything sail to, fall to, or in any other way reach this earth, without being smashed into fine particles by the impact?
This earth is supposed to rip space at a rate of about nineteen miles a second.
Concepts smash when one tries to visualize such an accomplishment.
Now, three times over, we shall have other aspects of this one mystery of the local sky. First we shall take up data upon seeming relation between a region of this earth that is subject to earthquakes, or so-called earthquakes, and appearances in the sky of this especial region, and the repeating falls of objects and substances from this local sky and nowhere else at the times.
We have had records of quakes that occurred at Irkutsk, Siberia, and of stones that fell from the sky to Irkutsk. Upon March 8, 1829, a severe quake, preceded by clattering sounds, was felt at Irkutsk. There was something in the sky. Dr. Erman, the geologist, was in Irkutsk, at the time. In the
Report of the British Association,
1854-20, it is said that, in Dr. Erman’s opinion, the sounds that preceded the quake were in the sky.
The situation at Comrie, Perthshire, is similar. A stone fell, May 17, 1830, in the “earthquake region” around Comrie. It fell at Perth, 22 miles from Comrie. See
Fletcher’s List,
p. 100. Upon Feb. 15, 1837, a black powder fell upon the Comrie region
(Edin. New Phil. Jour.,
31-293). Oct. 12, 1839—a quake at Comrie. According to the Rev. M. Walker, of Comrie, the sky, at the time, was “peculiarly strange and alarming, and appeared as if hung with sackcloth.” In Mallet’s Catalogue
(Rept. B.A.,
1854-290) it is said that, throughout the month of October, shocks were felt at Comrie, sometimes slight and sometimes severe—“like distant thunder or reports of artillery”—“the noise sometimes seemed to be high in the air, and was often heard without any sensible shock.” Upon the 23rd of October, occurred the most violent quake in the whole series of phenomena at Comrie. See the
Edin. New Phil. Jour.,
vol. 32. All data in this publication were collected by David Milne. According to the Rev. M. Maxton, of Foulis Manse, ten miles from Comrie, rattling sounds were heard in the sky, preceding the shock that was felt. In vol. 33, p. 373, of the
Journal,
someone who lived seven miles from Comrie is quoted: “In every case, I am inclined to say that the sound proceeded not from underground. The sound seemed high in the air.” Someone who lived at Gowrie, forty miles from Comrie, is quoted: “The most general opinion seems to be that the noise accompanying the concussion proceeded from above.” See vol. 34, p. 87: another impression of explosion overhead and concussion underneath: “The noises heard first seemed to be in the air, and the rumbling sound in the earth.” Milne’s own conclusion—“It is plain that there are, connected with the earthquake shocks, sounds both in the earth and in the air, which are distinct and separate.” If, upon the 23rd of October, 1839, there was a tremendous shock, not of subterranean origin, but from a great explosion in the sky of Comrie, and if this be accepted, there will be concussions somewhere else. The “faults” of dogmas will open; there will be seismic phenomena in science. I have a feeling of a conventional survey of this Scottish sky: vista of a fair, blue, vacant expanse—our suspicions daub the impression with black alarms—but also do we project detonating stimulations into the fair and blue, but unoccupied and meaningless. One cannot pass this single occurrence by, considering it only in itself: it is one of a long series of quakes of the earth at Comrie and phenomena in the sky at Comrie. We have stronger evidence than the mere supposition of many persons, in and near Comrie, that, upon Oct. 23, 1839, something had occurred in the sky, because sounds seemed to come from the sky. Milne says that clothes, bleaching on the grass, were entirely covered with black particles which presumably had fallen from the sky. The shocks were felt in November: in November, according to Milne, a powder-like soot fell from the sky, upon Comrie and surrounding regions. In his report to the British Association, 1840, Milne, reviewing the phenomena from the year 1788, says: “Occasionally there was a fall of fine, black powder.”
Jan. 8, 1840—sounds like cannonading, at Comrie, and a crackling sound in the air, according to some of the residents. Whether they were sounds of quakes or concussions that followed explosions, 247 occurrences between Oct. 3, 1839, are listed in the
Edin. New Phil. Jour.,
32-107. It looks like bombardment, and like most persistent bombardment—from somewhere—and the frequent fall from the sky of the débris of explosions. Feb. 18, 1841—a shock and a fall of discolored rain at Comrie
(Edin. New Phil. Jour.,
35-148). See Roper’s
List of Earthquakes
—year after year, and the continuance of this seeming bombardment in one small part of the sky of this earth, though I can find records only of dates and no details. However, I think I have found record of a fall from the sky of débris of an explosion, more substantial than finely powdered soot, at Crieff, which is several miles from Comrie. In the
Amer. Jour. Sci.,
2-28-275, Prof. Shepard tells a circumstantial story of an object that looked like a lump of slag, or cinders, reported to have fallen at Crieff. Scientists had refused to accept the story, upon the grounds that the substance was not of “true meteoric material.” Prof. Shepard went to Crieff and investigated. He gives his opinion that possibly the object did fall from the sky. The story that he tells is that, upon the night of April 23, 1855, a young woman, in the home of Sir William Murray, Achterlyre House, Crieff, saw, or thought she saw, a luminous object falling, and picked it up, dropping it, because it was hot, or because she thought it was hot.
For a description, in a letter, presumably from Sir William Murray, or some member of his family, see
Year Book of Facts,
1856-273.
It is said that about twelve fragments of scorious matter, hot and emitting a sulphurous odor, had fallen.
In Ponton’s
Earthquakes,
p. 118, it is said that, upon the 8th of October, 1857, there had been, in Illinois, an earthquake, preceded by “a luminous appearance, described by some as a meteor and by others as vivid flashes of lightning.” Though felt in Illinois, the center of the disturbance was at St. Louis, Mo. One notes the misleading and the obscuring of such wording: in all contemporaneous accounts there is no such indefiniteness as one description by “some” and another notion by “others.” Something exploded terrifically in the sky, at St. Louis, and shook the ground “severely” or “violently,” at 4:20 a.m., Oct. 8, 1857. According to Timbs’
Year Book of Facts,
1858-271, “a blinding meteoric ball from the heavens” was seen. “A large and brilliant meteor shot across the heavens”
(St. Louis Intelligencer,
October 8). Of course the supposed earthquake was concussion from an explosion in the sky, but our own interest is in a series that is similar to others that we have recorded. According to the
New York Times,
October 12, a slight shock was said to have been felt four hours before the great concussion, and another three days before. But see Milne’s
Catalog of Destructive Earthquakes—
not a mention of anything that would lead one away from safe and standardized suppositions. See
Bull. Seis. Soc. Amer.,
3-68—here the “meteor” is mentioned, but there is no mention of the preceding concussions. Time after time, in a period of about three days, concussions were felt in and around St. Louis. One of these concussions, with its “sound like thunder or the roar of artillery”
(New York Times,
October 8) was from an explosion in the sky. If the others were of the same origin—how could detonating meteors so repeat in one small local sky, and nowhere else, if this earth be a moving body? If it be said that only by coincidence did a meteor explode over a region where there had been other quakes, here is the question:
How many times can we accept that explanation as to similar series?
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In the
Proceedings of the Society for Psychical Research,
19-144, a correspondent writes that, in Herefordshire, Sept. 24, 1854, upon a day that was “perfectly still, sky cloudless,” he had heard sounds like the discharges of heavy artillery, at intervals of about two minutes, continuing several hours. Again the “mystery of the local sky”—if these sounds did come from the sky. We have no data for thinking that they did.
In the London
Times,
Nov. 9, 1858, a correspondent writes that, in Cardiganshire, Wales, he had, in the autumn of 1855, often heard sounds like the discharges of heavy artillery, two or three reports rapidly, and then an interval of perhaps twenty minutes, also with long intervals, sometimes of days and sometimes of weeks, continuing throughout the winter of 1855-56. Upon the 3rd of November, 1858, he had heard the sounds again, repeatedly, and louder than they had been three years before. In the
Times,
November 12, someone else says that, at Dolgelly, he, too, had heard the “mysterious phenomenon,” on the 3rd of November. Someone else—that, upon October 13, he had heard the sounds at Swansea. “The reports, as if of heavy artillery, came from the west, succeeding each other at apparently regular intervals, during the greater part of the afternoon of that day. My impression was that the sounds might have proceeded from practicing at Milford, but I ascertained, the following day, that there had been no firing of any kind there.” Correspondent to the
Times,
November 26—that, with little doubt, the sounds were from artillery practice at Milford. He does not mention the investigation as to the sounds of October 13, but says that there had been cannon-firing, upon November 3rd, at Milford.
Times,
December 1—that most of the sounds could be accounted for as sounds of blasting in quarries.
Daily News,
November 16—that similar sounds had been heard, in 1848, in New Zealand, and were results of volcanic action.
Standard,
November 16—that the “mysterious noise” must have been from Devonport, where a sunken rock had been blown up. So, with at least variety these sounds were explained. But we learn that the series began before October 13. Upon the evening of September 28, in the Dartmoor District, at Crediton, a rumbling sound was heard. It was not supposed to be an earthquake, because no vibration of the ground was felt. It was thought that there had been an explosion of gunpowder. But there had been no such terrestrial explosion. About an hour later another explosive sound was heard. It was like all the other sounds, and in one place was thought to be distant cannonading—terrestrial cannonading. See
Quar. Jour. Geolog. Soc. of London,
vol. 15.
Somewhere near Barisal, Bengal, were occurring just such sounds as the sounds of Cardiganshire, which were like the sounds of Melida. In the
Proc. Asiatic Soc. of Bengal,
November, 1870, are published letters upon the Barisal Guns. One writer says that the sounds were probably booming of the surf. Someone else points out that the sounds, usually described as “explosive,” were heard too far inland to be traced to such origin. A clear, calm day, in December, 1871—in
Nature,
53-197, Mr. G.B. Scott writes that, in Bengal, he had heard “a dull, muffled boom, as if of distant cannon”—single detonations, and then two or three in quicker succession.
In the London
Times,
Jan. 20, 1860, several correspondents write as to a sound “resembling the discharge of a gun high in the air” that was heard near Reading, Berkshire, England, Jan. 17, 1860. See the
Times,
January 24th. To say that a meteor had exploded would, at present, well enough account for this phenomenon.
Sounds like those that were heard in Herefordshire, Sept. 24, 1854, were heard later. In the
English Mechanic,
100-279, it is said that, upon Nov. 9, 1862, the Rev. T. Webb, the astronomer, of Hardwicke, fifteen miles west of Hereford, heard sounds that he attributed to gunfire at Milford Haven, about 85 miles from Hardwicke. Upon Aug. 1, 1865, Mr. Webb saw flashes upon the horizon, at Hardwicke, and attributed them to gunfire at Tenby, upon occasion of a visit by Prince Arthur. Tenby, too, is about 85 miles from Hardwicke. There were other phenomena in a region centering around Hereford and Worcester. Upon Oct. 6, 1863, there was a disturbance that is now listed as an earthquake; but in the London newspapers so many reports upon this occurrence state that a great explosion had been thought to occur, and that the quake was supposed to be an earthquake of subterranean origin only after no terrestrial explosion could be heard of, that the phenomenon is of questionable origin. There was a similar concussion in about the same region, Oct. 30, 1868. Again the shock was widely attributed to a great explosion, perhaps in London, and again was supposed to have been an earthquake when no terrestrial explosion could be heard of.
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Arcana of Science,
1829-196:
That, near Mhow, India, Feb. 27, 1828, fell a stone “perfectly similar” to the stone that fell near Allahabad, in 1802, and a stone that fell near Mooradabad, in 1808. These towns are in the Northwestern Provinces of India.
I have looked at specimens of these stones, and in my view they are similar. They are of brownish rock, streaked and spotted with a darker brown. A stone that fell at Chandakopur, in the same general region, June 6, 1838, is like them. All are as much alike as “erratics” that, because they are alike, geologists ascribe to the same derivation, stationary relatively to the places in which they are found.
It seems acceptable that, upon July 15 and 17, 1822, and then upon a later date, unknown seeds fell from the sky to this earth. If these seeds did come from some other world, there is another mystery as well as that of repetition in a local sky of this earth. How could a volume of seeds remain in one aggregation; how could the seeds be otherwise than scattered from Norway to Patagonia, if they met in space this earth, and if this earth be rushing through space at a rate of nineteen miles a second? It may be that the seeds of 1822 fell again. According to Kaemtz
(Meteorology,
p. 465) yellowish brown corpuscles, some round, a few cylindrical, were found upon the ground, June, 1830, near Griesau, Silesia. Kaemtz says that they were tubercules from roots of a well-known Silesian plant—stalk of the plant dries up; heavy rain raises these tubercules to the ground—persons of a low order of mentality think that the things had fallen from the sky. Upon the night of March 24-25, 1852, a great quantity of seeds did fall from the sky, in Prussia, in Heinsberg, Erklenz, and Juliers, according to M. Schwann, of the University of Liege, in a communication to the Belgian Academy of Science
(La Belgique Horticole,
2-319).