n later took another
shot.
These are speculations that seem to me to be evil relatively to these
early years in the twentieth century--
Just now, I accept that this earth is--not round, of course: that is
very old-fashioned--but roundish, or, at least, that it has what is
called form of its own, and does revolve upon its axis, and in an orbit
around the sun. I only accept these old traditional notions--
And that above it are regions of suspension that revolve with it: from
which objects fall, by disturbances of various kinds, and then, later,
fall again, in the same place:
_Monthly Weather Review_, May, 1884-134:
Report from the Signal Service observer, at Bismarck, Dakota:
That, at 9 o'clock, in the evening of May 22, 1884, sharp sounds were
heard throughout the city, caused by a fall of flinty stones striking
against windows.
Fifteen hours later another fall of flinty stones occurred at Bismarck.
There is no report of stones having fallen anywhere else.
This is a thing of the ultra-damned. All Editors of scientific
publications read the _Monthly Weather Review_ and frequently copy from
it. The noise made by the stones of Bismarck, rattling against those
windows, may be in a language that aviators will some day interpret:
but it was a noise entirely surrounded by silences. Of this ultra-damned
thing, there is no mention, findable by me, in any other publication.
The size of some hailstones has worried many meteorologists--but not
text-book meteorologists. I know of no more serene occupation than that
of writing text-books--though writing for the _War Cry_, of the
Salvation Army, may be equally unadventurous. In the drowsy tranquillity
of a text-book, we easily and unintelligently read of dust particles
around which icy rain forms, hailstones, in their fall, then increasing
by accretion--but in the meteorological journals, we read often of
air-spaces nucleating hailstones--
But it's the size of the things. Dip a marble in icy water. Dip and dip
and dip it. If you're a resolute dipper, you will, after a while, have
an object the size of a baseball--but I think a thing could fall from
the moon in that length of time. Also the strata of them. The Maryland
hailstones are unusual, but a dozen strata have often been counted.
Ferrel gives an instance of thirteen strata. Such considerations led
Prof. Schwedoff to argue that some hailstones are not, and cannot, be
generated in this earth's atmosphere--tha
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