as doubtful; fall of bituminous matter, in Germany, March 8, 1798, listed by Greg. Lockyer (The Meteoric Hypothesis, p. 24) says that the substance that fell at the Cape of Good Hope, Oct. 13, 1838—about five cubic feet of it: substance so soft that it was cuttable with a knife—"after being experimented upon, it left a residue, which gave out a very bituminous smell."
And this inclusion of Lockyer's—so far as findable in all books that I have read—is, in books, about as close as we can get to our desideratum—that coal has fallen from the sky. Dr. Farrington, except with a brief mention, ignores the whole subject of the fall of carbonaceous matter from the sky. Proctor, in all of his books that I have read—is, in books, about as close as we can get to duction to the Study of Meteorites," p. 53) excommunicates with the admission that carbonaceous matter has been found in meteorites "in very minute quantities"—or my own suspicion is that it is possible to damn something else only by losing one's own soul—quasi-soul, of course.
Sci. Amer., 35-120:
That the substance that fell at the Cape of Good Hope "resembled a piece of anthracite coal more than anything else."
It's a mistake, I think: the resemblance is to bituminous coal—but it is from the periodicals that we must get our data. To the writers of books upon meteorites, it would be as wicked—by which we mean departure from the characters of an established species—quasi-established, of course—to say that coal has fallen from the sky, as would be, to something in a barnyard, a temptation that it climb a tree and catch a bird. Domestic things in a barnyard: and how wild things from forests outside seem to them. Or the homeopathist—but we shall shovel data of coal.
And, if over and over, we shall learn of masses of soft coal that have fallen upon this earth, if in no instance has it been asserted that the masses did not fall, but were upon the ground in the first place; if we have many instances, this time we turn down good and hard the mechanical reflex that these masses were carried from one place to another in whirlwinds, because we find it too difficult to accept that whirlwinds could so select, or so specialize in a peculiar substance. Among writers of books, the only one I know of who makes more than brief mention is Sir Robert Ball. He represents a still more antique orthodoxy, or is an exclusionist of the old type, still holding out against even meteorites. He cites several falls of carbonaceous matter, but with disregards that make for reasonable-
