The Science of Super-Geography--

And Science is a turtle that says that its own shell encloses all

things.

So the members of the British Association. To some of them Prof.

Schwedoff's ideas were like slaps on the back of an environment-denying

turtle: to some of them his heresy was like an offering of meat, raw and

dripping, to milk-fed lambs. Some of them bleated like lambs, and some

of them turled like turtles. We used to crucify, but now we ridicule:

or, in the loss of vigor of all progress, the spike has etherealized

into the laugh.

Sir William Thomson ridiculed the heresy, with the phantomosities of his

era:

That all bodies, such as hailstones, if away from this earth's

atmosphere, would have to move at planetary velocity--which would be

positively reasonable if the pronouncements of St. Isaac were anything

but articles of faith--that a hailstone falling through this earth's

atmosphere, with planetary velocity, would perform 13,000 times as much

work as would raise an equal weight of water one degree centigrade, and

therefore never fall as a hailstone at all; be more than

melted--super-volatalized--

These turls and these bleats of pedantry--though we insist that,

relatively to 1882, these turls and bleats should be regarded as

respectfully as we regard rag dolls that keep infants occupied and

noiseless--it is the survival of rag dolls into maturity that we object

to--so these pious and naive ones who believed that 13,000 times

something could have--that is, in quasi-existence--an exact and

calculable resultant, whereas there is--in quasi-existence--nothing that

can, except by delusion and convenience, be called a unit, in the first

place--whose devotions to St. Isaac required blind belief in formulas of

falling bodies--

Against data that were piling up, in their own time, of slow-falling

meteorites; "milk warm" ones admitted even by Farrington and Merrill; at

least one icy meteorite nowhere denied by the present orthodoxy, a datum

as accessible to Thomson, in 1882, as it is now to us, because it was an

occurrence of 1860. Beans and needles and tacks and a magnet. Needles

and tacks adhere to and systematize relatively to a magnet, but, if some

beans, too, be caught up, they are irreconcilables to this system and

drop right out of it. A member of the Salvation Army may hear over and

over data that seem so memorable to an evolutionist. It seems remarkable

that they do not influence him--one finds that he cannot remember them.

It is incredible that Sir William Thomson had never heard of

slow-falling, cold meteorites. It is simply that he had no power to

remember such irreconcilabilities.

And then Mr. Symons again. Mr. Symons was a man who probably did more

for the science of meteorology than did any other man of his time:

therefore he probably did more to hold back the science of meteorology

than did any other man of his time. In _Nature_, 41-135, Mr. Symons says

that Prof. Schwedoff's ideas are "very droll."

I think that even more amusing is our own acceptance that, not very far

above this earth's surface, is a region that will be the subject of a

whole new science--super-geography--with which we shall immortalize

ourselves in the resentments of the schoolboys of the future--

Pebbles and fragments of meteors and things from Mars and Jupiter and

Azuria: wedges, delayed messages, cannon balls, bricks, nails, coal and

coke and charcoal and offensive old cargoes--things that coat in ice in

some regions and things that get into areas so warm that they

putrefy--or that there are all the climates of geography in

super-geography. I shall have to accept that, floating in the sky of

this earth, there often are fields of ice as extensive as those on the

Arctic Ocean--volumes of water in which are many fishes and

frogs--tracts of land covered with caterpillars--

Aviators of the future. They fly up and up. Then they get out and walk.

The fishing's good: the bait's right there. They find messages from

other worlds--and within three weeks there's a big trade worked up in

forged messages. Sometime I shall write a guide book to the

Super-Sargasso Sea, for aviators, but just at present there wouldn't be

much call for it.

We now have more of our expression upon hail as a concomitant, or more

data of things that have fallen from the sky, with hail.

In general, the expression is:

These things may have been raised from some other part of the earth's

surface, in whirlwinds, or may not have fallen, and may have been upon

the ground, in the first place--but were the hailstones found with them,

raised from some other part of the earth's surface, or were the

hailstones upon the ground, in the first place?

As I said before, this expression is meaningless as to a few instances;

it is reasonable to think of some coincidence between the fall of hail

and the fall of other things: but, inasmuch as there have been a good

many instances,--we begin to suspect that this is not so much a book

we're writing as a sanitarium for overworked coincidences. If not

conceivably could very large hailstones and lumps of ice form in this

earth's atmosphere, and so then had to come from external regions, then

other things in or accompanying very large hailstones and lumps of ice

came from external regions--which worries us a little: we may be

instantly translated to the Positive Absolute.

_Cosmos_, 13-120, quotes a Virginia newspaper, that fishes said to have

been catfishes, a foot long, some of them, had fallen, in 1853, at

Norfolk, Virginia, with hail.

Vegetable debris, not only nuclear, but frozen upon the surfaces of

large hailstones, at Toulouse, France, July 28, 1874. (_La Science Pour

Tous_, 1874-270.)

Description of a storm, at Pontiac, Canada, July 11, 1864, in which it

is said that it was not hailstones that fell, but "pieces of ice, from

half an inch to over two inches in diameter" (_Canadian Naturalist_,

2-1-308):

"But the most extraordinary thing is that a respectable farmer, of

undoubted veracity, says he picked up a piece of hail, or ice, in the

center of which was a small green frog."

Storm at Dubuque, Iowa, June 16, 1882, in which fell hailstones and

pieces of ice (_Monthly Weather Review_, June, 1882):

"The foreman of the Novelty Iron Works, of this city, states that in two

large hailstones melted by him were found small living frogs." But the

pieces of ice that fell upon this occasion had a peculiarity that

indicates--though by as bizarre an indication as any we've had yet--that

they had been for a long time motionless or floating somewhere. We'll

take that up soon.

_Living Age_, 52-186:

That, June 30, 1841, fishes, one of which was ten inches long, fell at

Boston; that, eight days later, fishes and ice fell at Derby.

In Timb's _Year Book_, 1842-275, it is said that, at Derby, the fishes

had fallen in enormous numbers; from half an inch to two inches long,

and some considerably larger. In the _Athenaeum_, 1841-542, copied from

the Sheffield _Patriot_, it is said that one of the fishes weighed three

ounces. In several accounts, it is said that, with the fishes, fell many

small frogs and "pieces of half-melted ice." We are told that the frogs

and the fishes had been raised from some other part of the earth's

surface, in a whirlwind; no whirlwind specified; nothing said as to what

part of the earth's surface comes ice, in the month of July--interests

us that the ice is described as "half-melted." In the London _Times_,

July 15, 1841, it is said that the fishes were sticklebacks; that they

had fallen with ice and small frogs, many of which had survived the

fall. We note that, at Dunfermline, three months later (Oct. 7, 1841)

fell many fishes, several inches in length, in a thunderstorm. (London

_Times_, Oct. 12, 1841.)

Hailstones, we don't care so much about. The matter of stratification

seems significant, but we think more of the fall of lumps of ice from

the sky, as possible data of the Super-Sargasso Sea:

Lumps of ice, a foot in circumference, Derbyshire, England, May 12, 1811

(_Annual Register_, 1811-54); cuboidal mass, six inches in diameter,

that fell at Birmingham, 26 days later (Thomson, _Intro. to

Meteorology_, p. 179); size of pumpkins, Bangalore, India, May 22, 1851

(_Rept. Brit. Assoc._, 1855-35); masses of ice of a pound and a half

each, New Hampshire, Aug. 13, 1851 (Lummis, _Meteorology_, p. 129);

masses of ice, size of a man's head, in the Delphos tornado (Ferrel,

_Popular Treatise_, p. 428); large as a man's hand, killing thousands of

sheep, Texas, May 3, 1877 (_Monthly Weather Review_, May, 1877); "pieces

of ice so large that they could not be grasped in one hand," in a

tornado, in Colorado, June 24, 1877 (_Monthly Weather Review_, June,

1877); lumps of ice four and a half inches long, Richmond, England, Aug.

2, 1879 (_Symons' Met. Mag._, 14-100); mass of ice, 21 inches in

circumference that fell with hail, Iowa, June, 1881 (_Monthly Weather

Review_, June, 1881); "pieces of ice" eight inches long, and an inch and

a half thick, Davenport, Iowa, Aug. 30, 1882 (_Monthly Weather Review_,

Aug., 1882); lump of ice size of a brick; weight two pounds, Chicago,

July 12, 1883 (_Monthly Weather Review_, July, 1883); lumps of ice that

weighed one pound and a half each, India, May (?), 1888 (_Nature_,

37-42); lump of ice weighing four pounds, Texas, Dec. 6, 1893 (_Sc.

Am._, 68-58); lumps of ice one pound in weight, Nov. 14, 1901, in a

tornado, Victoria (_Meteorology of Australia_, p. 34).

Of course it is our acceptance that these masses not only accompanied

tornadoes, but were brought down to this earth by tornadoes.

Flammarion, _The Atmosphere_, p. 34:

Block of ice, weighing four and a half pounds that fell at Cazorta,

Spain, June 15, 1829; block of ice, weighing eleven pounds, at Cette,

France, October, 1844; mass of ice three feet long, three feet wide, and

more than two feet thick, that fell, in a storm, in Hungary, May 8,

1802.

_Scientific American_, 47-119:

That, according to the _Salina Journal_, a mass of ice weighing about 80

pounds had fallen from the sky, near Salina, Kansas, August, 1882. We

are told that Mr. W.J. Hagler, the North Santa Fe merchant became

possessor of it, and packed it in sawdust in his store.

London _Times_, April 7, 1860:

That, upon the 16th of March, 1860, in a snowstorm, in Upper Wasdale,

blocks of ice, so large that at a distance they looked like a flock of

sheep, had fallen.

_Rept. Brit. Assoc._, 1851-32:

That a mass of ice about a cubic yard in size had fallen at Candeish,

India, 1828.

Against these data, though, so far as I know, so many of them have never

been assembled together before, there is a silence upon the part of

scientific men that is unusual. Our Super-Sargasso Sea may not be an

unavoidable conclusion, but arrival upon this earth of ice from external

regions does seem to be--except that there must be, be it ever so faint,

a merger. It is in the notion that these masses of ice are only

congealed hailstones. We have data against this notion, as applied to

all our instances, but the explanation has been offered, and, it seems

to me, may apply in some instances. In the _Bull. Soc. Astro. de

France_, 20-245, it is said of blocks of ice the size of decanters that

had fallen at Tunis that they were only masses of congealed hailstones.

London _Times_, Aug. 4, 1857.

That a block of ice, described as "pure" ice, weighing 25 pounds, had

been found in the meadow of Mr. Warner, of Cricklewood. There had been a

storm the day before. As in some of our other instances, no one had seen

this object fall from the sky. It was found after the storm: that's all

that can be said about it.

Letter from Capt. Blakiston, communicated by Gen. Sabine, to the Royal

Society (_London Roy. Soc. Proc._, 10-468):

That, Jan. 14, 1860, in a thunderstorm, pieces of ice had fallen upon

Capt. Blakiston's vessel--that it was not hail. "It was not hail, but

irregular-shaped pieces of solid ice of different dimensions, up to the

size of half a brick."

According to the _Advertiser-Scotsman_, quoted by the Edinburgh _New

Philosophical Magazine_, 47-371, an irregular-shaped mass of ice fell at

Ord, Scotland, August, 1849, after "an extraordinary peal of thunder."

It is said that this was homogeneous ice, except in a small part, which

looked like congealed hailstones.

The mass was about 20 feet in circumference.

The story, as told in the London _Times_, Aug. 14, 1849, is that, upon

the evening of the 13th of August, 1849, after a loud peal of thunder, a

mass of ice said to have been 20 feet in circumference, had fallen upon

the estate of Mr. Moffat, of Balvullich, Ross-shire. It is said that

this object fell alone, or without hailstones.

Altogether, though it is not so strong for the Super-Sargasso Sea, I

think this is one of our best expressions upon external origins. That

large blocks of ice could form in the moisture of this earth's

atmosphere is about as likely as that blocks of stone could form in a

dust whirl. Of course, if ice or water comes to this earth from external

sources, we think of at least minute organisms in it, and on, with our

data, to frogs, fishes; on to anything that's thinkable, coming from

external sources. It's of great importance to us to accept that large

lumps of ice have fallen from the sky, but what we desire most--perhaps

because of our interest in its archaeologic and palaeontologic

treasures--is now to be through with tentativeness and probation, and

to take the Super-Sargasso Sea into full acceptance in our more advanced

fold of the chosen of this twentieth century.

In the _Report of the British Association_, 1855-37, it is said that, at

Poorhundur, India, Dec. 11, 1854, flat pieces of ice, many of them

weighing several pounds--each, I suppose--had fallen from the sky. They

are described as "large ice-flakes."

Vast fields of ice in the Super-Arctic regions, or strata, of the

Super-Sargasso Sea. When they break up, their fragments are flake-like.

In our acceptance, there are aerial ice-fields that are remote from this

earth; that break up, fragments grinding against one another, rolling in

vapor and water, of different constituency in different regions, forming

slowly as stratified hailstones--but that there are ice-fields near this

earth, that break up into just such flat pieces of ice as cover any pond

or river when ice of a pond or river is broken, and are sometimes soon

precipitated to the earth, in this familiar flat formation.

_Symons' Met. Mag._, 43-154:

A correspondent writes that, at Braemar, July 2, 1908, when the sky was

clear overhead, and the sun shining, flat pieces of ice fell--from

somewhere. The sun was shining, but something was going on somewhere:

thunder was heard.

Until I saw the reproduction of a photograph in the _Scientific

American_, Feb. 21, 1914, I had supposed that these ice-fields must be,

say, at least ten or twenty miles away from this earth, and invisible,

to terrestrial observers, except as the blurs that have so often been

reported by astronomers and meteorologists. The photograph published by

the _Scientific American_ is of an aggregation supposed to be clouds,

presumably not very high, so clearly detailed are they. The writer says

that they looked to him like "a field of broken ice." Beneath is a

picture of a conventional field of ice, floating ordinarily in water.

The resemblance between the two pictures is striking--nevertheless, it

seems to me incredible that the first of the photographs could be of an

aerial ice-field, or that gravitation could cease to act at only a mile

or so from this earth's surface--

Unless:

The exceptional: the flux and vagary of all things.

Or that normally this earth's gravitation extends, say, ten or fifteen

miles outward--but that gravitation must be rhythmic.

Of course, in the pseudo-formulas of astronomers, gravitation as a fixed

quantity is essential. Accept that gravitation is a variable force, and

astronomers deflate, with a perceptible hissing sound, into the

punctured condition of economists, biologists, meteorologists, and all

the others of the humbler divinities, who can admittedly offer only

insecure approximations.

We refer all who would not like to hear the hiss of escaping arrogance,

to Herbert Spencer's chapters upon the rhythm of all phenomena.

If everything else--light from the stars, heat from the sun, the winds

and the tides; forms and colors and sizes of animals; demands and

supplies and prices; political opinions and chemic reactions and

religious doctrines and magnetic intensities and the ticking of clocks;

and arrival and departure of the seasons--if everything else is

variable, we accept that the notion of gravitation as fixed and

formulable is only another attempted positivism, doomed, like all other

illusions of realness in quasi-existence. So it is intermediatism to

accept that, though gravitation may approximate higher to invariability

than do the winds, for instance, it must be somewhere between the

Absolutes of Stability and Instability. Here then we are not much

impressed with the opposition of physicists and astronomers, fearing, a

little mournfully, that their language is of expiring sibilations.

So then the fields of ice in the sky, and that, though usually so far

away as to be mere blurs, at times they come close enough to be seen in

detail. For description of what I call a "blur," see _Pop. Sci. News_,

February, 1884--sky, in general, unusually clear, but, near the sun, "a

white, slightly curdled haze, which was dazzlingly bright."

We accept that sometimes fields of ice pass between the sun and the

earth: that many strata of ice, or very thick fields of ice, or

superimposed fields would obscure the sun--that there have been

occasions when the sun was eclipsed by fields of ice:

Flammarion, _The Atmosphere_, p. 394:

That a profound darkness came upon the city of Brussels, June 18, 1839:

There fell flat pieces of ice, an inch long.

Intense darkness at Aitkin, Minn., April 2, 1889: sand and "solid chunks

of ice" reported to have fallen (_Science_, April 19, 1889).

In _Symons' Meteorological Magazine_, 32-172, are outlined rough-edged

but smooth-surfaced pieces of ice that fell at Manassas, Virginia, Aug.

10, 1897. They look as much like the roughly broken fragments of a

smooth sheet of ice--as ever have roughly broken fragments of a smooth

sheet of ice looked. About two inches across, and one inch thick. In

_Cosmos_, 3-116, it is said that, at Rouen, July 5, 1853, fell

irregular-shaped pieces of ice, about the size of a hand, described as

looking as if all had been broken from one enormous block of ice. That,

I think, was an aerial iceberg. In the awful density, or almost absolute

stupidity of the 19th century, it never occurred to anybody to look for

traces of polar bears or of seals upon these fragments.

Of course, seeing what we want to see, having been able to gather these

data only because they are in agreement with notions formed in advance,

we are not so respectful to our own notions as to a similar impression

forced upon an observer who had no theory or acceptance to support. In

general, our prejudices see and our prejudices investigate, but this

should not be taken as an absolute.

_Monthly Weather Review_, July, 1894:

That, from the Weather Bureau, of Portland, Oregon, a tornado, of June

3, 1894, was reported.

Fragments of ice fell from the sky.

They averaged three to four inches square, and about an inch thick. In

length and breadth they had the smooth surfaces required by our

acceptance: and, according to the writer in the _Review_, "gave the

impression of a vast field of ice suspended in the atmosphere, and

suddenly broken into fragments about the size of the palm of the hand."

This datum, profoundly of what we used to call the "damned," or before

we could no longer accept judgment, or cut and dried condemnation by

infants, turtles, and lambs, was copied--but without comment--in the

_Scientific American_, 71-371.

Our theology is something like this:

Of course we ought to be damned--but we revolt against adjudication by

infants, turtles, and lambs.

We now come to some remarkable data in a rather difficult department of

super-geography. Vast fields of aerial ice. There's a lesson to me in

the treachery of the imaginable. Most of our opposition is in the

clearness with which the conventional, but impossible, becomes the

imaginable, and then the resistant to modifications. After it had become

the conventional with me, I conceived clearly of vast sheets of ice, a

few miles above this earth--then the shining of the sun, and the ice

partly melting--that note upon the ice that fell at Derby--water

trickling and forming icicles upon the lower surface of the ice sheet. I

seemed to look up and so clearly visualized those icicles hanging like

stalactites from a flat-roofed cave, in white calcite. Or I looked up at

the under side of an aerial ice-lump, and seemed to see a papillation

similar to that observed by a calf at times. But then--but then--if

icicles should form upon the under side of a sheet of aerial ice, that

would be by the falling of water toward this earth; an icicle is of

course an expression of gravitation--and, if water melting from ice

should fall toward this earth, why not the ice itself fall before an

icicle could have time to form? Of course, in quasi-existence, where

everything is a paradox, one might argue that the water falls, but the

ice does not, because the ice is heavier--that is, in masses. That

notion, I think, belongs in a more advanced course than we are taking at

present.

Our expression upon icicles:

A vast field of aerial ice--it is inert to this earth's gravitation--but

by universal flux and variation, part of it sags closer to this earth,

and is susceptible to gravitation--by cohesion with the main mass, this

part does not fall, but water melting from it does fall, and forms

icicles--then, by various disturbances, this part sometimes falls in

fragments that are protrusive with icicles.

Of the ice that fell, some of it enclosing living frogs, at Dubuque,

Iowa, June 16, 1882, it is said (_Monthly Weather Review_, June, 1882)

that there were pieces from one to seventeen inches in circumference,

the largest weighing one pound and three-quarters--that upon some of

them were icicles half an inch in length. We emphasize that these

objects were not hailstones.

The only merger is that of knobby hailstones, or of large hailstones

with protuberances wrought by crystallization: but that is no merger

with terrestrial phenomena, and such formations are unaccountable to

orthodoxy; or it is incredible that hail could so crystallize--not

forming by accretion--in the fall of a few seconds. For an account of

such hailstones, see _Nature_, 61-594. Note the size--"some of them the

size of turkeys' eggs."

It is our expression that sometimes the icicles themselves have fallen,

as if by concussion, or as if something had swept against the under side

of an aerial ice floe, detaching its papillations.

_Monthly Weather Review_, June, 1889:

That, at Oswego, N.Y., June 11, 1889, according to the Turin (N.Y.)

_Leader_, there fell, in a thunderstorm, pieces of ice that "resembled

the fragments of icicles."

_Monthly Weather Review_, 29-506:

That on Florence Island, St. Lawrence River, Aug. 8, 1901, with ordinary

hail, fell pieces of ice "formed like icicles, the size and shape of

lead pencils that had been cut into sections about three-eighths of an

inch in length."

So our data of the Super-Sargasso Sea, and its Arctic region: and, for

weeks at a time, an ice field may hang motionless over a part of this

earth's surface--the sun has some effect upon it, but not much until

late in the afternoon, I should say--part of it has sagged, but is held

up by cohesion with the main mass--whereupon we have such an occurrence

as would have been a little uncanny to us once upon a time--or fall of

water from a cloudless sky, day after day, in one small part of this

earth's surface, late in the afternoon, when the sun's rays had had time

for their effects:

_Monthly Weather Review_, October, 1886:

That, according to the Charlotte _Chronicle_, Oct. 21, 1886, for three

weeks there had been a fall of water from the sky, in Charlotte, N.C.,

localized in one particular spot, every afternoon, about three o'clock;

that, whether the sky was cloudy or cloudless, the water or rain fell

upon a small patch of land between two trees and nowhere else.

This is the newspaper account, and, as such, it seems in the depths of

the unchosen, either by me or any other expression of the Salvation

Army. The account by the Signal Service observer, at Charlotte,

published in the _Review_, follows:

"An unusual phenomenon was witnessed on the 21st: having been informed

that, for some weeks prior to date, rain had been falling daily, after 3

P.M., on a particular spot, near two trees, corner of 9th and D streets,

I visited the place, and saw precipitation in the form of rain drops at

4:47 and 4:55 P.M., while the sun was shining brightly. On the 22nd, I

again visited the place, and from 4:05 to 4:25 P.M., a light shower of

rain fell from a cloudless sky.... Sometimes the precipitation falls

over an area of half an acre, but always appears to center at these two

trees, and when lightest occurs there only."

14

We see conventionally. It is not only that we think and act and speak

and dress alike, because of our surrender to social attempt at Entity,

in which we are only super-cellular. We see what it is "proper" that we

should see. It is orthodox enough to say that a horse is not a horse, to

an infant--any more than is an orange an orange to the unsophisticated.

It's interesting to walk along a street sometimes and look at things and

wonder what they'd look like, if we hadn't been taught to see horses and

trees and houses as horses and trees and houses. I think that to

super-sight they are local stresses merging indistinguishably into one

another, in an all-inclusive nexus.

I think that it would be credible enough to say that many times have

Monstrator and Elvera and Azuria crossed telescopic fields of vision,

and were not even seen--because it wouldn't be proper to see them; it

wouldn't be respectable, and it wouldn't be respectful: it would be

insulting to old bones to see them: it would bring on evil influences

from the relics of St. Isaac to see them.

But our data:

Of vast worlds that are orbitless, or that are navigable, or that are

adrift in inter-planetary tides and currents: the data that we shall

have of their approach, in modern times, within five or six miles of

this earth--

But then their visits, or approaches, to other planets, or to other of

the few regularized bodies that have surrendered to the attempted Entity

of this solar system as a whole--

The question that we can't very well evade:

Have these other worlds, or super-constructions, ever been seen by

astronomers?

I think there would not be much approximation to realness in taking

refuge in the notion of astronomers who stare and squint and see only

that which it is respectable and respectful to see. It is all very well

to say that astronomers are hypnotics, and that an astronomer looking at

the moon is hypnotized by the moon, but our acceptance is that the

bodies of this present expression often visit the moon, or cross it, or

are held in temporary suspension near it--then some of them must often

have been within the diameter of an astronomer's hypnosis.

Our general expression:

That, upon the oceans of this earth, there are regularized vessels, but

also that there are tramp vessels:

That, upon the super-ocean, there are regularized planets, but also that

there are tramp worlds:

That astronomers are like mercantile purists who would deny commercial

vagabondage.

Our acceptance is that vast celestial vagabonds have been excluded by

astronomers, primarily because their irresponsibilities are an affront

to the pure and the precise, or to attempted positivism; and secondarily

because they have not been seen so very often. The planets steadily

reflect the light of the sun: upon this uniformity a system that we call

Primary Astronomy has been built up; but now the subject-matter of

Advanced Astronomy is data of celestial phenomena that are sometimes

light and sometimes dark, varying like some of the satellites of

Jupiter, but with a wider range. However, light or dark, they have been

seen and reported so often that the only important reason for their

exclusion is--that they don't fit in.

With dark bodies that are probably external to our own solar system, I

have, in the provincialism that no one can escape, not much concern.

Dark bodies afloat in outer space would have been damned a few years

ago, but now they're sanctioned by Prof. Barnard--and, if he says

they're all right, you may think of them without the fear of doing

something wrong or ridiculous--the close kinship we note so often

between the evil and the absurd--I suppose by the ridiculous I mean the

froth of evil. The dark companion of Algol, for instance. Though that's

a clear case of celestial miscegenation, the purists, or positivists,

admit that's so. In the _Proceedings of the National Academy of

Science_, 1915-394, Prof. Barnard writes of an object--he calls it an

"object"--in Cephus. His idea is that there are dark, opaque bodies

outside this solar system. But in the _Astrophysical Journal_, 1916-1,

he modifies into regarding them as "dark nebulae." That's not so

interesting.

We accept that Venus, for instance, has often been visited by other

worlds, or by super-constructions, from which come ciders and coke and

coal; that sometimes these things have reflected light and have been

seen from this earth--by professional astronomers. It will be noted that

throughout this chapter our data are accursed Brahmins--as, by hypnosis

and inertia, we keep on and keep on saying, just as a good many of the

scientists of the 19th century kept on and kept on admitting the power

of the system that preceded them--or Continuity would be smashed.

There's a big chance here for us to be instantaneously translated to the

Positive Absolute--oh, well--

What I emphasize here is that our damned data are observations by

astronomers of the highest standing, excommunicated by astronomers of

similar standing--but backed up by the dominant spirit of their era--to

which all minds had to equilibrate or be negligible, unheard, submerged.

It would seem sometimes, in this book, as if our revolts were against

the dogmatisms and pontifications of single scientists of eminence. This

is only a convenience, because it seems necessary to personify. If we

look over _Philosophical Transactions_, or the publications of the Royal

Astronomical Society, for instance, we see that Herschel, for instance,

was as powerless as any boy stargazer, to enforce acceptance of any

observation of his that did not harmonize with the system that was

growing up as independently of him and all other astronomers, as a phase

in the development of an embryo compels all cells to take on appearances

concordantly with the design and the predetermined progress and schedule

of the whole.

Visitors to Venus:

Evans, _Ways of the Planets_, p. 140:

That, in 1645, a body large enough to look like a satellite was seen

near Venus. Four times in the first half of the 18th century, a similar

observation was reported. The last report occurred in 1767.

A large body has been seen--seven times, according to _Science Gossip_,

1886-178--near Venus. At least one astronomer, Houzeau, accepted these

observations and named the--world, planet, super-construction--"Neith."

His views are mentioned "in passing, but without endorsement," in the

_Trans. N.Y. Acad._, 5-249.

Houzeau or someone writing for the magazine-section of a Sunday

newspaper--outer darkness for both alike. A new satellite in this solar

system might be a little disturbing--though the formulas of Laplace,

which were considered final in his day, have survived the admittance of

five or six hundred bodies not included in those formulas--a satellite

to Venus might be a little disturbing, but would be explained--but a

large body approaching a planet--staying awhile--going away--coming back

some other time--anchoring, as it were--

Azuria is pretty bad, but Azuria is no worse than Neith.

_Astrophysical Journal_, 1-127:

A light-reflecting body, or a bright spot near Mars: seen Nov. 25, 1894,

by Prof. Pickering and others, at the Lowell Observatory, above an

unilluminated part of Mars--self-luminous, it would seem--thought to

have been a cloud--but estimated to have been about twenty miles away

from the planet.

Luminous spot seen moving across the disk of Mercury, in 1799, by

Harding and Schroeter. (_Monthly Notices of the R.A.S._, 38-338.)

In the first Bulletin issued by the Lowell Observatory, in 1903, Prof.

Lowell describes a body that was seen on the terminator of Mars, May

20, 1903. On May 27, it was "suspected." If still there, it had moved,

we are told, about 300 miles--"probably a dust cloud."

Very conspicuous and brilliant spots seen on the disk of Mars, October

and November, 1911. (_Popular Astronomy_, Vol. 19, No. 10.)

So one of them accepted six or seven observations that were in

agreement, except that they could not be regularized, upon a

world--planet--satellite--and he gave it a name. He named it "Neith."

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