ness that earthy matter may have been caught up by whirlwinds and flung down somewhere else. If he had given a full list, he would be called upon to explain the special affinity of whirlwinds for a special kind of coal. He does not give a full list. We shall have all that's findable, and we shall see that against this disease we're writing, the homeopathist's prescription availeth not. Another exclusionist was Prof. Lawrence Smith. His psycho-tropism was to respond to all reports of carbonaceous matter falling from the sky, by saying that this damned matter had been deposited upon things of the chosen by impact with this earth. Most of our data antedate him, or were contemporaneous with him, or were as accessible to him as to us. In his attempted positivism it is simply—and beautifully—disregarded that, according to Berthelot, Berzelius, Cloez, Wohler and others these masses are not merely coated with carbonaceous matter, but are carbonaceous throughout, or are permeated throughout. How any one could so resolutely and dogmatically and beautifully and blindly hold out, would puzzle us were it not for our acceptance that only to think is to exclude and include; and to exclude some things that have as much right to come in as have the included—that to have an opinion upon any subject is to be a Lawrence Smith—because there is no definite subject.
Dr. Walter Flight (Eclectic Magazine, 89-71) says, of the substance that fell near Alais, France, March 15, 1806, that it "emits a faint bituminous substance" when heated, according to the observations of Berzelius and a commission appointed by the French Academy. This time we have not the reluctances expressed in such words as "like" and "resembling." We are told that this substance is "an earthy kind of coal."
As to "minute quantities" we are told that the substance that fell at the Cape of Good Hope has in it a little more than a quarter of organic matter, which, in alcohol, gives the familiar reaction of yellow, resinous matter. Other instances given by Dr. Flight are:
Carbonaceous matter that fell in 1840, in Tennessee; Cranbourne, Australia, 1861; Montauban, France, May 14, 1864 (twenty masses, some of them as large as a human head; of a substance that "resembled a dull-colored earthy lignite"); Goalpara, India, about 1867 (about 8 per cent of a hydrocarbon); at Ornans, France, July 11, 1868; substance with "an organic, combustible ingredient," at Hessle, Sweden, Jan. 1, 1860.
Knowledge, 4-134:
