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Authors: Charles Fort
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12 and 13, 1902, occurred the greatest fall of matter in the history of Australia. Upon the 14th of November, it “rained mud,” in Tasmania. It was of course attributed to Australian whirlwinds, but, according to the Monthly Weather Review, 32-365, there was a haze all the way to the Philippines, also as far as Hong Kong. It may be that this phenomenon had no especial relation with the even more tremendous fall of matter that occurred in Europe, February, 1903.
For several days, the south of England was a dumping ground—from somewhere.
If you’d like to have a chemist’s opinion, even though it’s only a chemist’s opinion, see the report of the meeting of the Royal Chemical Society, April 2, 1903. Mr. E.G. Clayton read a paper upon some of the substance that had fallen from the sky, collected by him. The Sahara explanation applies mostly to falls that occur in southern Europe. Farther away, the conventionalists are a little uneasy: for instance, the Editor of the Monthly Weather Review, 29-121, says of a red rain that fell near the coast of Newfoundland, early in 1890: “It would be very remarkable if this was Sahara dust.” Mr. Clayton said that the matter examined by him was “merely wind-borne dust from the roads and lanes of Wessex.” This opinion is typical of all scientific opinion—or theological opinion—or feminine opinion—all very well except for what it disregards. The most charitable thing I can think of—because I think it gives us a broader tone to relieve our malices with occasional charities—is that Mr. Clayton had not heard of the astonishing extent of this fall—had covered the Canary Islands, on the 19th, for instance. I think, myself, that in 1903, we passed through the remains of a powdered world—left over from an ancient interplanetary dispute, brooding in space like a red resentment ever since. Or, like every other opinion, the notion of dust from Wessex turns into a provincial thing when we look it over.
To think is to conceive incompletely, because all thought relates only to the local. We metaphysicians, of course, like to have the notion that we think of the unthinkable.
As to opinions, or pronouncements, I should say, because they always have such an authoritative air, of other chemists, there is an analysis in Nature, 68-54, giving water and organic matter at 9.08 percent. It’s that carrying out of fractions that’s so convincing. The substance is identified as sand from the Sahara.
The vastness of this fall. In Nature, 68-65, we are told that it had occurred in Ireland, too. The Sahara, of course—because, prior to February 19, there had been dust storms in the Sahara—disregarding that in that great region there’s always, in some part of it, a dust storm. However, just at present, it does look reasonable that dust had come from Africa, via the Canaries.
The great difficulty that authoritativeness has to contend with is some other authoritativeness. When an infallibility clashes with a pontification—
They explain.
Nature, March 5, 1903:
Another analysis—36 percent organic matter.
Such disagreements don’t look very well, so, in Nature, 68-109, one of the differing chemists explains. He says that his analysis was of muddy rain, and the other was of sediment of rain—
We’re quite ready to accept excuses from the most high, though I do wonder whether we’re quite so damned as we were, if we find ourselves in a gracious and tolerant mood toward the powers that condemn—but the tax that now comes upon our good manners and unwillingness to be too severe—
Nature, 68-223:
Another chemist. He says it was 23.49 percent water and organic matter.
He “identifies” this matter as sand from an African desert—but after deducting organic matter—
But you and I could be “identified” as sand from an African desert, after deducting all there is to us except sand—
Why we cannot accept that this fall was of sand from the Sahara, omitting the obvious
For several days, the south of England was a dumping ground—from somewhere.
If you’d like to have a chemist’s opinion, even though it’s only a chemist’s opinion, see the report of the meeting of the Royal Chemical Society, April 2, 1903. Mr. E.G. Clayton read a paper upon some of the substance that had fallen from the sky, collected by him. The Sahara explanation applies mostly to falls that occur in southern Europe. Farther away, the conventionalists are a little uneasy: for instance, the Editor of the Monthly Weather Review, 29-121, says of a red rain that fell near the coast of Newfoundland, early in 1890: “It would be very remarkable if this was Sahara dust.” Mr. Clayton said that the matter examined by him was “merely wind-borne dust from the roads and lanes of Wessex.” This opinion is typical of all scientific opinion—or theological opinion—or feminine opinion—all very well except for what it disregards. The most charitable thing I can think of—because I think it gives us a broader tone to relieve our malices with occasional charities—is that Mr. Clayton had not heard of the astonishing extent of this fall—had covered the Canary Islands, on the 19th, for instance. I think, myself, that in 1903, we passed through the remains of a powdered world—left over from an ancient interplanetary dispute, brooding in space like a red resentment ever since. Or, like every other opinion, the notion of dust from Wessex turns into a provincial thing when we look it over.
To think is to conceive incompletely, because all thought relates only to the local. We metaphysicians, of course, like to have the notion that we think of the unthinkable.
As to opinions, or pronouncements, I should say, because they always have such an authoritative air, of other chemists, there is an analysis in Nature, 68-54, giving water and organic matter at 9.08 percent. It’s that carrying out of fractions that’s so convincing. The substance is identified as sand from the Sahara.
The vastness of this fall. In Nature, 68-65, we are told that it had occurred in Ireland, too. The Sahara, of course—because, prior to February 19, there had been dust storms in the Sahara—disregarding that in that great region there’s always, in some part of it, a dust storm. However, just at present, it does look reasonable that dust had come from Africa, via the Canaries.
The great difficulty that authoritativeness has to contend with is some other authoritativeness. When an infallibility clashes with a pontification—
They explain.
Nature, March 5, 1903:
Another analysis—36 percent organic matter.
Such disagreements don’t look very well, so, in Nature, 68-109, one of the differing chemists explains. He says that his analysis was of muddy rain, and the other was of sediment of rain—
We’re quite ready to accept excuses from the most high, though I do wonder whether we’re quite so damned as we were, if we find ourselves in a gracious and tolerant mood toward the powers that condemn—but the tax that now comes upon our good manners and unwillingness to be too severe—
Nature, 68-223:
Another chemist. He says it was 23.49 percent water and organic matter.
He “identifies” this matter as sand from an African desert—but after deducting organic matter—
But you and I could be “identified” as sand from an African desert, after deducting all there is to us except sand—
Why we cannot accept that this fall was of sand from the Sahara, omitting the obvious
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