Page:The Book of the Damned (Fort, 1919).djvu/91

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BOOK OF THE DAMNED
85

Amer. Jour. Sci., 1-32-199:

That, according to testimony taken before a magistrate, a fall occurred, Feb. 19, 1830, near Feridpoor, India, of many fishes, of various sizes—some whole and fresh and others "mutilated and putrefying." Our reflex to those who would say that, in the climate of India, it would not take long for fishes to putrefy, is—that high in the air, the climate of India is not torrid. Another peculiarity of this fall is that some of the fishes were much larger than others. Or to those who hold out for segregation in a whirlwind, or that objects, say, twice as heavy as others would be separated from the lighter, we point out that some of these fishes were twice as heavy as others.

In the Journal of the Asiatic Society of Bengal, 2-650, depositions of witnesses are given:

"Some of the fish were fresh, but others were rotten and without heads."

'Among the number which I got, five were fresh and the rest stinking and headless."

They remind us of His Grace's observation of some pages back.

According to Dr. Buist, some of these fishes weighed one and a half pounds each and others three pounds.

A fall of fishes, at Futtepoor, India, May 16, 1833:

"They were all dead and dry." (Dr. Buist, Living Age, 52-186.)

India is far away: about 1830 was long ago:

Nature, Sept. 19, 1918-46:

A correspondent writes, from the Dove Marine Laboratory, Cuttercoats, England, that, at Hindon, a suburb of Sunderland, Aug. 24, 1918, hundreds of small fishes, identified as sand eels, had fallen——

Again the small area: about 60 by 30 yards.

The fall occurred during a heavy rain that was accompanied by thunder—or indications of disturbance aloft—but by no visible lightning. The sea is close to Hindon, but if you try to think of these fishes having described a trajectory in a whirlwind from the ocean, consider this remarkable datum:

That, according to witnesses, the fall upon this small area, occupied ten minutes.

I can not think of a clearer indication of a direct fall from a stationary source.

And: