The Book of the Damned Part 20

Fall, with snow, at Orenburg, Russia, Dec. 14, 1830, of a mult.i.tude of small, black insects, said to have been gnats, but also said to have had flea-like motions. (_Amer. Jour. Sci._, 1-22-375.)

Large number of worms found in a snowstorm, upon the surface of snow about four inches thick, near Sangerfield, N.Y., Nov. 18, 1850 (_Scientific American_, 6-96). The writer thinks that the worms had been brought to the surface of the ground by rain, which had fallen previously.

_Scientific American_, Feb. 21, 1891:

"A puzzling phenomenon has been noted frequently in some parts of the Valley Bend District, Randolph County, Va., this winter. The crust of the snow has been covered two or three times with worms resembling the ordinary cut worms. Where they come from, unless they fall with the snow is inexplicable." In the _Scientific American_, March 7, 1891, the Editor says that similar worms had been seen upon the snow near Utica, N.Y., and in Oneida and Herkimer Counties; that some of the worms had been sent to the Department of Agriculture at Washington. Again two species, or polymorphism. According to Prof. Riley, it was not polymorphism, "but two distinct species"--which, because of our data, we doubt. One kind was larger than the other: color-differences not distinctly stated. One is called the larvae of the common soldier beetle and the other "seems to be a variety of the bronze cut worm." No attempt to explain the occurrence in snow.

Fall of great numbers of larvae of beetles, near Mortagne, France, May, 1858. The larvae were inanimate as if with cold. (_Annales Societe Entomologique de France_, 1858.)

_Trans. Ent. Soc. of London_, 1871-183, records "snowing of larvae," in Silesia, 1806; "appearance of many larvae on the snow," in Saxony, 1811; "larvae found alive on the snow," 1828; larvae and snow which "fell together," in the Eifel, Jan. 30, 1847; "fall of insects," Jan.

24, 1849, in Lithuania; occurrence of larvae estimated at 300,000 on the snow in Switzerland, in 1856. The compiler says that most of these larvae live underground, or at the roots of trees; that whirlwinds uproot trees, and carry away the larvae--conceiving of them as not held in ma.s.ses of frozen earth--all as neatly detachable as currants in something. In the _Revue et Magasin de Zoologie_, 1849-72, there is an account of the fall in Lithuania, Jan. 24, 1849--that black larvae had fallen in enormous numbers.

Larvae thought to have been of beetles, but described as "caterpillars,"

not seen to fall, but found crawling on the snow, after a snowstorm, at Warsaw, Jan. 20, 1850. (_All the Year Round_, 8-253.)

Flammarion (_The Atmosphere_, p. 414) tells of a fall of larvae that occurred Jan. 30, 1869, in a snowstorm, in Upper Savoy: "They could not have been hatched in the neighborhood, for, during the days preceding, the temperature had been very low"; said to have been of a species common in the south of France. In _La Science Pour Tous_, 14-183, it is said that with these larvae there were developed insects.

_L'Astronomie_, 1890-313:

That, upon the last of January, 1890, there fell, in a great tempest, in Switzerland, incalculable numbers of larvae: some black and some yellow; numbers so great that hosts of birds were attracted.

Altogether we regard this as one of our neatest expressions for external origins and against the whirlwind explanation. If an exclusionist says that, in January, larvae were precisely and painstakingly picked out of frozen ground, in incalculable numbers, he thinks of a tremendous force--disregarding its refinements: then if origin and precipitation be not far apart, what becomes of an infinitude of other debris, conceiving of no time for segregation?

If he thinks of a long translation--all the way from the south of France to Upper Savoy, he may think then of a very fine sorting over by differences of specific gravity--but in such a fine selection, larvae would be separated from developed insects.

As to differences in specific gravity--the yellow larvae that fell in Switzerland January, 1890, were three times the size of the black larvae that fell with them. In accounts of this occurrence, there is no denial of the fall.

Or that a whirlwind never brought them together and held them together and precipitated them and only them together--

That they came from Genesistrine.

There's no escape from it. We'll be persecuted for it. Take it or leave it--

Genesistrine.

The notion is that there is somewhere aloft a place of origin of life relatively to this earth. Whether it's the planet Genesistrine, or the moon, or a vast amorphous region super-jacent to this earth, or an island in the Super-Sarga.s.so Sea, should perhaps be left to the researches of other super--or extra--geographers. That the first unicellular organisms may have come here from Genesistrine--or that men or anthropomorphic beings may have come here before amoebae: that, upon Genesistrine, there may have been an evolution expressible in conventional biologic terms, but that evolution upon this earth has been--like evolution in modern j.a.pan--induced by external influences; that evolution, as a whole, upon this earth, has been a process of population by immigration or by bombardment. Some notes I have upon remains of men and animals encysted, or covered with clay or stone, as if fired here as projectiles, I omit now, because it seems best to regard the whole phenomenon as a tropism--as a geotropism--probably atavistic, or vestigial, as it were, or something still continuing long after expiration of necessity; that, once upon a time, all kinds of things came here from Genesistrine, but that now only a few kinds of bugs and things, at long intervals, feel the inspiration.

Not one instance have we of tadpoles that have fallen to this earth. It seems reasonable that a whirlwind could scoop up a pond, frogs and all, and cast down the frogs somewhere else: but, then, more reasonable that a whirlwind could scoop up a pond, tadpoles and all--because tadpoles are more numerous in their season than are the frogs in theirs: but the tadpole-season is earlier in the spring, or in a time that is more tempestuous. Thinking in terms of causation--as if there were real causes--our notion is that, if X is likely to cause Y, but is more likely to cause Z, but does not cause Z, X is not the cause of Y. Upon this quasi-sorites, we base our acceptance that the little frogs that have fallen to this earth are not products of whirlwinds: that they came from externality, or from Genesistrine.

I think of Genesistrine in terms of biologic mechanics: not that somewhere there are persons who collect bugs in or about the last of January and frogs in July and August, and bombard this earth, any more than do persons go through northern regions, catching and collecting birds, every autumn, then casting them southward.

But atavistic, or vestigial, geotropism in Genesistrine--or a million larvae start crawling, and a million little frogs start hopping--knowing no more what it's all about than we do when we crawl to work in the morning and hop away at night.

I should say, myself, that Genesistrine is a region in the Super-Sarga.s.so Sea, and that parts of the Super-Sarga.s.so Sea have rhythms of susceptibility to this earth's attraction.

8

I accept that, when there are storms, the d.a.m.nedest of excluded, excommunicated things--things that are leprous to the faithful--are brought down--from the Super-Sarga.s.so Sea--or from what for convenience we call the Super-Sarga.s.so Sea--which by no means has been taken into full acceptance yet.

That things are brought down by storms, just as, from the depths of the sea things are brought up by storms. To be sure it is orthodoxy that storms have little, if any, effect below the waves of the ocean--but--of course--only to have an opinion is to be ignorant of, or to disregard a contradiction, or something else that modifies an opinion out of distinguishability.

_Symons' Meteorological Magazine_, 47-180:

That, along the coast of New Zealand, in regions not subject to submarine volcanic action, deep-sea fishes are often brought up by storms.

Iron and stones that fall from the sky; and atmospheric disturbances:

"There is absolutely no connection between the two phenomena."

(_Symons._)

The orthodox belief is that objects moving at planetary velocity would, upon entering this earth's atmosphere, be virtually unaffected by hurricanes; might as well think of a bullet swerved by someone fanning himself. The only trouble with the orthodox reasoning is the usual trouble--its phantom-dominant--its basing upon a myth--data we've had, and more we'll have, of things in the sky having no independent velocity.

There are so many storms and so many meteors and meteorites that it would be extraordinary if there were no concurrences. Nevertheless so many of these concurrences are listed by Prof. Baden-Powell (_Rept.

Brit. a.s.soc._, 1850-54) that one--notices.

See _Rept. Brit. a.s.soc._, 1860--other instances.

The famous fall of stones at Siena, Italy, 1794--"in a violent storm."

See _Greg's Catalogues_--many instances. One that stands out is--"bright ball of fire and light in a hurricane in England, Sept. 2, 1786." The remarkable datum here is that this phenomenon was visible forty minutes.

That's about 800 times the duration that the orthodox give to meteors and meteorites.

See the _Annual Register_--many instances.

In _Nature_, Oct. 25, 1877, and the London _Times_, Oct. 15, 1877, something that fell in a gale of Oct. 14, 1877, is described as a "huge ball of green fire." This phenomenon is described by another correspondent, in _Nature_, 17-10, and an account of it by another correspondent was forwarded to _Nature_ by W.F. Denning.

There are so many instances that some of us will revolt against the insistence of the faithful that it is only coincidence, and accept that there is connection of the kind called causal. If it is too difficult to think of stones and metallic ma.s.ses swerved from their courses by storms, if they move at high velocity, we think of low velocity, or of things having no velocity at all, hovering a few miles above this earth, dislodged by storms, and falling luminously.

But the resistance is so great here, and "coincidence" so insisted upon that we'd better have some more instances:

Aerolite in a storm at St. Leonards-on-sea, England, Sept. 17, 1885--no trace of it found (_Annual Register_, 1885); meteorite in a gale, March 1, 1886, described in the _Monthly Weather Review_, March, 1886; meteorite in a thunderstorm, off coast of Greece, Nov. 19, 1899 (_Nature_, 61-111); fall of a meteorite in a storm, July 7, 1883, near Lachine, Quebec (_Monthly Weather Review_, July, 1883); same phenomenon noted in _Nature_, 28-319; meteorite in a whirlwind, Sweden, Sept. 24, 1883 (_Nature_, 29-15).

_London Roy. Soc. Proc._, 6-276:

A triangular cloud that appeared in a storm, Dec. 17, 1852; a red nucleus, about half the apparent diameter of the moon, and a long tail; visible 13 minutes; explosion of the nucleus.

Nevertheless, in _Science Gossip_, n.s., 6-65, it is said that, though meteorites have fallen in storms, no connection is supposed to exist between the two phenomena, except by the ignorant peasantry.

But some of us peasants have gone through the _Report of the British a.s.sociation_, 1852. Upon page 239, Dr. Buist, who had never heard of the Super-Sarga.s.so Sea, says that, though it is difficult to trace connection between the phenomena, three aerolites had fallen in five months, in India, during thunderstorms, in 1851 (may have been 1852).

For accounts by witnesses, see page 229 of the _Report_.

Or--we are on our way to account for "thunderstones."

It seems to me that, very strikingly here, is borne out the general acceptance that ours is only an intermediate existence, in which there is nothing fundamental, or nothing final to take as a positive standard to judge by.