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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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